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                  <text>(SFM) Igneous Suite -- St. Francois Mountains, Southeastern Missouri</text>
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                  <text>This collection is composed of igneous volcanic and intrusive rocks from the St. Francois Mountains of Missouri. The variation within the collection can be used to explain the geologic history of the area. The St. Francois Mountains batholith was formed by granitic intrusions into Precambrian rhyolites, tuffs, and breccias. Then basalt, diabase, and porphyritic intrusions cut the granitoids.</text>
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                  <text>Western Minerals, Inc.</text>
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                  <text>Start here:Â &lt;br /&gt;&lt;br /&gt;Bickford, M.E. and Mose, D.G., 1974, Geochronology of Precambrian rocks, St. Francois Mountains, South eastern Missouri: GSA Special Papers 1975, v. 165, p. 1-48 doi: &lt;a href="http://dx.doi.org/10.1130/SPE165-p1" target="_blank"&gt;http://dx.doi.org/10.1130/SPE165-p1&lt;br /&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Early study of the geochronology of the Precambrian rocks within the St. Francois mountains. Provides further insight upon the sequence discussed in the dscription.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Meert, J.G. and Stuckey, W., 2002, Revisiting the paleomagnetism of the 1.476 Ga St. Francois Mountains igneous province, Missouri: Tectonics v. 21, Issue 2, p. 1-19 doi: &lt;a href="http://dx.doi.org/10.1029/2000TC001265%20" target="_blank"&gt;http://dx.doi.org/10.1029/2000TC001265 &lt;br /&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Information acquired from paleomagnestism studies of the St. Francois igneous provence has proven fruitful for determining an acient paleomagnetic pole for Laurentia.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Menuge, J.F, Brewer, T.S., and Seeger, C.M., 2002, Petrogenesis of metaluminous A-type rhyolites from the St. Francois Mountains, Missouri and the Mesoproterozoic evolution of the southern Laurentian Margin: Precambrian Research, volume 113, issues 3-4, p. 269-291 doi: &lt;a href="http//dx.doi.org/10.1016/S0301-9268(01)00211-X%20" target="_blank"&gt;http//dx.doi.org/10.1016/S0301-9268(01)00211-X &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Trace elemental analysis of Precambrian rocks from the SFM provide insight into the condition of crystallization and the elemental constituents which played a role into the interesting history of this rhyolitic provence.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Rohs, R. C, and Van Schmus, W.R., 2006, Isotopic connection between basement rocks exposed in the St. Francois Mountains and the arbucks Mountains southern mid-continent, North America: International Journal of Earth Sciences, volume 96, Issue 4, p. 599-611 &lt;br /&gt;doi: &lt;a href="http://dx.doi.org/10.1007/s00531-006-0123-5" target="_blank"&gt;http://dx.doi.org/10.1007/s00531-006-0123-5&lt;br /&gt;&lt;/a&gt;
&lt;ul&gt;&lt;li&gt;&lt;span style="color:#000000;"&gt;Radiometric study of the SFM provence and the Arbuckle mountains of southern Oklahoma suggests a common source.Â &lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Wenner, D. and Taylor Jr., H.P., 1976, Oxygen and hydrogen isotope studies of a Precambian granite-rhyolite terrane, ST. Francois Mountains, southeastern Missouri: Geological Society of America bulletin v. 87, no. 11, p.1587-1598 &lt;br /&gt;doi: &lt;a href="http://dx.doi.org/10.1130/0016-7606" target="_blank"&gt;http://dx.doi.org/10.1130/0016-7606&lt;br /&gt;&lt;/a&gt;
&lt;ul&gt;&lt;li&gt;Isotopic analysis of oxygen isotope content within mineral grains within the Precambrian rhyolitic rocks of the SFM yields data that suggests Precambrian oceans were similar to modern day meteoric oceans.&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>Brown Mountain intrusive Rhyolite</text>
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                <text>Hand Sample: Porphyritic orange-pink rhyolite. Dominantly potassium feldspar with some black crystals. Weathers to brown-black and yellow-brown.  </text>
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                <text>Thin Section, XPL: Fine-grained, well-weathered quartz and alkaline feldspar interspersed with fine-grained rectangular inclusions of mixed material. Opaques present.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/15"&gt;St. Francois Mountains&lt;/a&gt;</text>
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                  <text>(FM) Flysch Stratigraphic Suite -- Molasse Basin, Switzerland </text>
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                  <text>Flysch is dominantly a turbidite succession, alternating sandstone and shale 100mm to rarely 100m in syntectonic accumulations. With a rising landmass shedding clastic debris into "deep" troughs, oversteepening of sediments along the shelf or actual tilting of the shell initiated turbidity currents flows deeper into the marine basin. There may be hundreds of these units in a given section. Nappes then over rode the soft sediments, locally producing strong deformational structures in the flysch sediments.Â &lt;br /&gt;&lt;br /&gt;The nappes shed their debris into fresh marine environments in great fans with large accumulations of coarse conglomerates. A molasse section may be a thousand meters thick. Molasse comprises a clastic sedimentary succession in a post-tectonic environment. &lt;br /&gt;&lt;br /&gt;Flysch and molasse both have sedimentatlogical as well as tectonic implications associated with their appearance in an outcrop. Â &lt;br /&gt;&lt;br /&gt;Dr. Trumpy at the Geological Institute in Zurich suggested specific localities for collecting and arranged for Dr. Hanspeter and Mr. Freeman to take me into the field on successive days. Later, Mr. Freeman spent several days in order to procure this suite. &lt;br /&gt;&lt;br /&gt;A set of kodachrome slides is available and should be used with the specimens to put the rocks into relationships seen in the field. There are 11 slide specimens. All slide specimens were photographed in PPL and XPL.</text>
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                  <text>Western Minerals, inc.</text>
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                <elementText elementTextId="17995">
                  <text>&lt;strong&gt;Start Here:&lt;/strong&gt; &lt;br /&gt;Eynatten, H.V., 2003, Petrology and chemistry of sandstones from the Swiss Molasse Basin: an archive of the Oligocene to Miocene of the Central Alps: Sedimentology, v.50, p.703-724. &lt;a href="http://dx.doi.org/10.1046/j.1365-1309.2003.00571.x"&gt;http://dx.doi.org/10.1046/j.1365-1309.2003.00571.x&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Fluvial sandstones from the Swiss Molasse Basin were analyzed for sandstone framework composition, heavy minerals, whole-rock geochemistry and detrital chrome spinel chemistry to understand its provenance.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional resources:&lt;/strong&gt; &lt;br /&gt;Schlunegger, F., Matter, A., Burbank, D.W., and Â Klaper, E.M., 1997, Magnetostratigraphic constraints on relationships between evolution of the central Swiss Molasse Basin and Alpine orogenic events: Geological Society of America Bulletin, v.109, p.225-241. &lt;a href="http://dx.doi.org/10.1130/0016-7606(1997)1092.3.CO;2%20"&gt;http://dx.doi.org/10.1130/0016-7606(1997)1092.3.CO;2 &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Magnetostratigraphic chronologies, together with lithostratigraphic, sedimentological, and petrological data enable detailed reconstruction of the Oligocene to Miocene history of the North Alpine foreland basin in relation to specific orogenic events and exhumation of the Alps.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Sinclair, H.D., 1997, Flysch to molasses transition in peripheral foreland basins; the role of the passive margin versus slab breakoff: Geology, v.25, p.1123-1126. &lt;a href="http://dx.doi.org/10.1130/0091-7613(1997)0252.3.CO;2%20"&gt;http://dx.doi.org/10.1130/0091-7613(1997)0252.3.CO;2 &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;It is proposed that slab breakoff may have been responsible for the increased sediment supply that resulted in the flysch to molasse transition in the North Alpine foreland basin, and that this provides an alternative to the passive margin model.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Spiegel, C., Siebel, W., Frisch, W., and Berner, Z., 2002, Nd and Sr isotopic ratios and trace element geochemistry of epidote from the Swiss Molasse Basin as provenance indicators; implications for the reconstruction of the echumation history of the Central Alps: Chemical Geology, v.189, p.231-250.&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Uses a combination of events to explain the geodynamic scenario of large-scale lateral extension processes affecting the Central Alps in post-collisional times.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Willet, S.D. and Schlunegger, F., 2010, The last phase of deposition in the Swiss Molasse Basin; from foredeep to negative-alpha basin: Basin Research, v.22, p.623-639. &lt;a href="http://dx.doi.org/10.1111/j.1365-2117.2009.00435.x%20"&gt;http://dx.doi.org/10.1111/j.1365-2117.2009.00435.x &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Simple analytical theory for the necessary conditions for such a negative-alpha basin to develop and be maintained.&lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>Typical turbidite sequence rocks (predominantly clastics with some evidence of carbonate input) </text>
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                  <text>In the Late Eocene, the area subsided again and developed into the Molasse Basin. </text>
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                  <text>Purchased by Western Minerals Inc.</text>
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                  <text>Turbidite sequences and carbonate pulses of deposition in a basin.</text>
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                  <text>The collection consists of a variety of shale, sandstones and conglomerates that illustrate sediment trapped in a molasse basin. </text>
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                  <text>Oct. 10, 2013</text>
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                <text>Fine grained relatively soft calcareous sandstone.&lt;br /&gt;&lt;br /&gt; Thin Section Fine angular grains with fairly close packing characterize this thin section, with unusually sharp angles. Sample is still clay dominated.</text>
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                <text>Western Minerals, lnc.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/13"&gt;Flysch Molasse Suite&lt;/a&gt;</text>
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                <text>Sternenberg, Germany</text>
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                <text>Purchased from Western Minerals, Inc.</text>
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                <text>Oct., 11, 2013</text>
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                <text>Mesozoic </text>
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                  <text>(ADK) Anorthosite-Charnockite and Metamorphic Suite --&#13;
 Adirondack Mountains, New York</text>
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                  <text>The Adirondack Mountains of northern New York State are underlain by approximately 20,000 square miles of complexly deformed, high grade metamorphic rocks which are believed to represent a southern outlier of the much larger Grenville Province.The Adirondacks can be divided into the "Lowlands" and the "Highlands" . The Lowlands comprise the northwestern quarter of the belt and are characterized by amphibolite facies metamorphism. The Highlands appear to consist entirely of granulite facies rocks.  All rocks in this suite have been collected from the Highlands and predominantly from the southern quarter of the Adirondacks.  &#13;
&#13;
This suite of rocks is designed to be representative of the Highlands in general. Therefore it includes both metasedimentary and metaigneous rocks.  The latter are very common throughout the Adirondacks and contain the often-discussed anorthosite-charnockite suite of rocks. Almost all rocks in the Adirondack Highlands are strongly foliated. This is the result of intense polyphase deformation that has affected this area.&#13;
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                  <text>Western Minerals Inc.</text>
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                <elementText elementTextId="17808">
                  <text>&lt;strong&gt;Start here:Â &lt;br /&gt;&lt;/strong&gt;McLelland, J., and Selleck, B.W.,2011,Â Megacrystic Gore Mountain-type garnets in the Adirondack Highlands; age, origin, and tectonic implications:Geosphere, v.7, no. 5, p.1194-1208, doi:Â &lt;a href="http://dx.doi.org/10.1130/GES00683.1" target="_blank"&gt;10.1130/GES00683.1&lt;/a&gt;.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article describes the formation of the megacrystic garnet amphibolites in the Gore Mountain section of the Adirondack Mountains. The authors conclude that three main factors influenced the garnet development: collapse of the Ottawan orogeny, intrusion of Lyon Mountain Granite, and fluid-related alteration at high temperature.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;McLelland, J.M., Bickford, M.E., Hill, B.M., Clechenko, C.C., Valley, J.W., and Hamilton, M.A., 2004,Â Direct dating of Adirondack Massif anorthosite by U-Pb SHRIMP analysis of igneous zircon; implications for AMCG complexes:Â Geological Society of America Bulletin, v.116, no. 11-12, p.1299-1317, doi:Â &lt;a href="http://dx.doi.org/10.1130/B25482.1" target="_blank"&gt;10.1130/B25482.1&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article describes techniques used to more accurately date the Adirondack Massif anorthosite.The authors concluded that the massifsÂ &lt;span&gt;constitute a single, composite anorthosite-mangerite-charnockite-granite (AMCG) suite intruded at ca. 1155 Ma. Although the rock suite is considered to be coeval, the authors conclude the rocks are not comagmatic.&lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;McLelland, J., Bickford, M.E., Spear, F., and Storm, L., 2002, Geology and geochronolgy of the eastern Adirondacks inÂ &lt;span&gt;New England Intercollegiate Geological Conference, 94th, New York State Geological Association 74th: guidebook for field trips in New York and Vermont : Lake George, New York&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This field trip guide provides for nine stops in the eastern Adirondacks. It also include some thin sections images and zircon images from sample rocks of the field trip stops.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;McLelland, J., Daly, J.S., and McLelland, J.M., 1996,Â The Grenville orogenic cycle (ca. 1350-1000 Ma); an Adirondack perspective: Tectonophysics, v.265, issue 1-2, p.1-28, doi: &lt;a href="http://dx.doi.org/10.1016/S0040-1951(96)00144-8" target="_blank"&gt;10.1016/S0040-1951(96)00144-8&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article provides a detailed geochronological account of the Grenville orogeny (ca. 1350-1000 Ma) with emphasis on the impact it had on the formation of the Adirondack Mountains.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;McLelland, J., Lewis, A., and Moore, L., 1994,Â Composition and petrogenesis of oxide-, apatite-rich gabbronorites associated with Proterozoic anorthosite massifs: examples from the Adirondack Mountains, New York: Contributions to Mineralogy and Petrology, v.116, p.225-238, doi:Â &lt;a href="http://dx.doi.org/10.1007/BF00310702" target="_blank"&gt;10.1007/BF00310702&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article investigates the occurence of oxide-, apatite-rich gabbronorites with anorthosite massifs of the Adirondacks. The authors describe a multilple-step process of plagioclase crystal fractionation that ultimately leads to high concentrations of P, Fe, and Ti.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;New York State Geological Survey&lt;br /&gt;&lt;a href="http://www.nysm.nysed.gov/nysgs/nygeology/mineralogy/adirondacks/index.html"&gt;http://www.nysm.nysed.gov/nysgs/nygeology/mineralogy/adirondacks/index.html&lt;br /&gt;&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;The NYS Geological Survey is a division of the New York State Museum system. This web page provides some details about the Adirondack Highlands and pictures of various minerals found in this region.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Regan, S.P., Chiarenzelli, J.R., McLelland,Â J.M., and Cousens, B. L., 2011,Â Evidence for an enriched asthenospheric source for coronitic metagabbros in the Adirondack Highlands: Geosphere, v.7, issue 3, p.&lt;span&gt;Â 694-709, doi:Â &lt;a href="http://dx.doi.org/10.1130/GES00629.1" target="_blank"&gt;10.1130/GES00629.1&lt;/a&gt;.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article describes the formation of coronitc metagabbros through tectonic processes involving the asthenosphere. Through geochemical and isotopic analyses, the authors provide a timeline of tectonic and petrologic events that supports an asthenospheric source for coronitic metagabbros.&lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>1980</text>
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              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
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                <elementText elementTextId="17815">
                  <text>The Adirondack Mountains were formed approximately 1.1- 1.3 billion years ago during the Grenville Orogeny (Precambrian eon, Proterozic era).</text>
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              <name>Accrual Method</name>
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                <elementText elementTextId="17816">
                  <text>Purchased from Western Minerals Inc. </text>
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              </elementTextContainer>
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                  <text>This rock suite was collected from the Adirondack Mountains located in the northeastern part of New York State.</text>
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              <text>Blue Mountain Lake Formation</text>
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              <text>1</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/7"&gt;Anorthosite-Charnockite and Metmorphic Suite-Adirondack Mountains, New York&lt;/a&gt;</text>
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                <text>Adirondack Highlands-collected on NY Route 30 from a large road cut 3.1 miles east of Speculator, NY.</text>
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                <text>Minerals found in the calcsilicate facies contain quartz, diopside, enstatitic pyroxene, tremolite, calcite, and phlogopite. However, only a few thin sections have been found to contain all phases. In some specimens, the pyroxene is close to 100% enstatite. The assemblage may be due to the reaction tremolite=diopside+ enstatite + quartz +fluid. This reaction discussed by Boyd, "Hydrothermal Investigations of Amphiboles," in Abelson, p.377-396.&#13;
Thin section shows calcite, diopside and phlogopite.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/4ee10b43b24c8c4757ea46f6ecefea71.pdf"&gt;NWME Rock Suite&lt;/a&gt;</text>
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                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Ernst, W.G., 2015, Franciscan geologic history constrained by tectonic/olistostromal high-grade metamafic blocks in the iconic California Mesozoic-Cenozoic accretionary complex: American Mineralogist, v. 100, p. 6-13.Â &lt;a href="http://dx.doi.org/10.2138/am-2015-4850" target="_blank"&gt;&lt;span&gt;doi:Â &lt;/span&gt;&lt;span class="slug-doi"&gt;10.2138/am-2015-4850&lt;/span&gt;&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This source supplies useful information on the low temperature, high pressure environment in which these rocks formed.Â &lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;Barnes, J., Eldam, R., Lee, C.T., Errico, J., Loewy, S., and Cisneros, M., 2013, Petrogenesis of serpentinites from the Franciscan Complex, western California, USA: Lithos, v. 178, p. 143-157.Â &lt;a class="S_C_ddDoi" href="http://dx.doi.org/10.1016/j.lithos.2012.12.018" target="_blank"&gt;doi:10.1016/j.lithos.2012.12.018&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Describes the petrogenesis of serpentine as seen in one of the items in the collection (Fr-4).&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Cooper, F., Platt, J., and Anczkiewicz, R., 2011, Constraints on early Franciscan subduction rates from 2-D thermal modeling: Earth and Planetary Science Letters, v. 312, p. 69-79. doi:&lt;a href="http://dx.doi.org/10.1016/j.epsl.2011.09.051"&gt;10.1016/j.epsl.2011.09.051&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper suggests that the rate of subduction in this area may have been five times lower than previous studies have found.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Ghatak, A., Basu, A., and Wakabayashi, J., 2013, Implications of Franciscan Complex graywacke geochemistry for sediment transport, provenance determination, burial-exposure duration, and fluid exchange with cosubducted metabasites: Tectonics, v. 32, p. 1480-1492. doi:Â &lt;a href="http://dx.doi.org/10.1002/tect.20078"&gt;10.1002/tect.20078&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article states that the europium anomalies of the greywacke samples suggest provenance from the Sierra Nevada batholith.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Langenheim, V., Jachens, R., Wentworth, C., and McLaughlin, R., 2013, Previously unrecognized regional structure of the Coastal Belt of the Franciscan Complex, northern California, revealed by magnetic data: Geosphere, v. 9, p. 1514-1529. doi:Â &lt;a href="http://dx.doi.org/10.1130/GES00942.1"&gt;10.1130/GES00942.1&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;&lt;span&gt;Using magnetic data, this article provides an overview of the regional structure of the Franciscan Complex.&lt;/span&gt;&lt;/li&gt;
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                  <text>Western Minerals, Inc. - Collection was supervised by Dr. Frederick C. Marshall, Assistant Professor of Geology at Principia College.</text>
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                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Ernst, W.G., 2015, Franciscan geologic history constrained by tectonic/olistostromal high-grade metamafic blocks in the iconic California Mesozoic-Cenozoic accretionary complex: American Mineralogist, v. 100, p. 6-13.Â &lt;a href="http://dx.doi.org/10.2138/am-2015-4850" target="_blank"&gt;&lt;span&gt;doi:Â &lt;/span&gt;&lt;span class="slug-doi"&gt;10.2138/am-2015-4850&lt;/span&gt;&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This source supplies useful information on the low temperature, high pressure environment in which these rocks formed.Â &lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;Barnes, J., Eldam, R., Lee, C.T., Errico, J., Loewy, S., and Cisneros, M., 2013, Petrogenesis of serpentinites from the Franciscan Complex, western California, USA: Lithos, v. 178, p. 143-157.Â &lt;a class="S_C_ddDoi" href="http://dx.doi.org/10.1016/j.lithos.2012.12.018" target="_blank"&gt;doi:10.1016/j.lithos.2012.12.018&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Describes the petrogenesis of serpentine as seen in one of the items in the collection (Fr-4).&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Cooper, F., Platt, J., and Anczkiewicz, R., 2011, Constraints on early Franciscan subduction rates from 2-D thermal modeling: Earth and Planetary Science Letters, v. 312, p. 69-79. doi:&lt;a href="http://dx.doi.org/10.1016/j.epsl.2011.09.051"&gt;10.1016/j.epsl.2011.09.051&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper suggests that the rate of subduction in this area may have been five times lower than previous studies have found.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Ghatak, A., Basu, A., and Wakabayashi, J., 2013, Implications of Franciscan Complex graywacke geochemistry for sediment transport, provenance determination, burial-exposure duration, and fluid exchange with cosubducted metabasites: Tectonics, v. 32, p. 1480-1492. doi:Â &lt;a href="http://dx.doi.org/10.1002/tect.20078"&gt;10.1002/tect.20078&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article states that the europium anomalies of the greywacke samples suggest provenance from the Sierra Nevada batholith.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Langenheim, V., Jachens, R., Wentworth, C., and McLaughlin, R., 2013, Previously unrecognized regional structure of the Coastal Belt of the Franciscan Complex, northern California, revealed by magnetic data: Geosphere, v. 9, p. 1514-1529. doi:Â &lt;a href="http://dx.doi.org/10.1130/GES00942.1"&gt;10.1130/GES00942.1&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;&lt;span&gt;Using magnetic data, this article provides an overview of the regional structure of the Franciscan Complex.&lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Mitchell, R.H., 2014, Primary and secondary niobium mineral deposits associated with carbonatites:Â Ore Geology Reviews,Â v. 64, p.Â 626-641,Â doi:10.1016/j.oregeorev.2014.03.010. &lt;a title="Full Article." href="http://dx.doi.org/10.1016/j.oregeorev.2014.03.010"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Focuses specifically on the formation of niobium in carbonatites but includes an excellent baseline description of carbonatites.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Nash, W.P., 1972, Mineralogy and Petrology of the Iron HillÂ &lt;span class="search-result-highlight"&gt;Carbonatite&lt;/span&gt;Â Complex, Colorado: Geological Society of America Bulletin, &lt;span class="cit-vol"&gt;&lt;span class="cit-sep cit-sep-before-article-vol"&gt;v.Â &lt;/span&gt;83&lt;span class="cit-sep cit-sep-after-article-vol"&gt;, p.Â &lt;/span&gt;&lt;/span&gt;&lt;span class="cit-pages"&gt;&lt;span class="cit-first-page"&gt;1361&lt;/span&gt;&lt;span class="cit-sep"&gt;-&lt;/span&gt;&lt;span class="cit-last-page"&gt;1382&lt;/span&gt;&lt;/span&gt;, doi:Â 10.1130/0016-7606(1972)83[1361:MAPOTI]2.0.CO;2. &lt;a title="Full Article." href="http://dx.doi.org/10.1130/0016-7606(1972)83%5B1361:MAPOTI%5D2.0.CO;2"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Bulk rock chemistry description &amp;amp; maps/diagrams showing the location of rocks in the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;
Temple, R.K., Grogran, R.M.,Â &lt;span&gt;1965, C&lt;span&gt;arbonatite and related alkalic rocks at powder horn, Colorado:Â &lt;span&gt;Economic geology and the bulletin of the Society of Economic Geologists, v. 60, p.Â &lt;span&gt;672-692, doi:Â 10.2113/gsecongeo.60.4.672. &lt;a title="Full Article" href="http://dx.doi.org/10.2113/gsecongeo.60.4.672."&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Basic information regarding the structure, geochemistry, and petrogenesis of the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Van Gosen, B. S., Lowers, H. A., 2007, Iron Hill (Powderhorn)Â carbonatiteÂ complex, Gunnison County, CO; a potential source of several uncommon mineral resources: Mining Engineering, v. 59, p. 56-62, doi: N/AÂ &lt;a title="Abstract" href="http://me.smenet.org/abstract.cfm?articleID=1143&amp;amp;page=56"&gt;Abstract.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Mineral resource potential: titanium, iron, vermiculite, vanadium, and nephaline.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Olson, J.C., Hedland, D.C., &lt;span&gt;1981&lt;/span&gt;, &lt;span&gt;Alkalic rocks and resources of thorium and associated elements in the Powderhorn District, Gunnison County, Colorado&lt;/span&gt;: &lt;span&gt;USGS Numbered Series&lt;/span&gt;, Professional Paper , v. &lt;span&gt;1049, &lt;span&gt;p. C1-C34&lt;/span&gt;Â &lt;/span&gt;Â doi: N/A. &lt;a title="Full Article" href="http://pubs.usgs.gov/pp/1049c/report.pdf"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Extensive report by the USGS regarding rock type and history of formation (geologic ages).&lt;/li&gt;
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Mitchell, R.H., 2014, Primary and secondary niobium mineral deposits associated with carbonatites:Â Ore Geology Reviews,Â v. 64, p.Â 626-641,Â doi:10.1016/j.oregeorev.2014.03.010. &lt;a title="Full Article." href="http://dx.doi.org/10.1016/j.oregeorev.2014.03.010"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Focuses specifically on the formation of niobium in carbonatites but includes an excellent baseline description of carbonatites.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Nash, W.P., 1972, Mineralogy and Petrology of the Iron HillÂ &lt;span class="search-result-highlight"&gt;Carbonatite&lt;/span&gt;Â Complex, Colorado: Geological Society of America Bulletin, &lt;span class="cit-vol"&gt;&lt;span class="cit-sep cit-sep-before-article-vol"&gt;v.Â &lt;/span&gt;83&lt;span class="cit-sep cit-sep-after-article-vol"&gt;, p.Â &lt;/span&gt;&lt;/span&gt;&lt;span class="cit-pages"&gt;&lt;span class="cit-first-page"&gt;1361&lt;/span&gt;&lt;span class="cit-sep"&gt;-&lt;/span&gt;&lt;span class="cit-last-page"&gt;1382&lt;/span&gt;&lt;/span&gt;, doi:Â 10.1130/0016-7606(1972)83[1361:MAPOTI]2.0.CO;2. &lt;a title="Full Article." href="http://dx.doi.org/10.1130/0016-7606(1972)83%5B1361:MAPOTI%5D2.0.CO;2"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Bulk rock chemistry description &amp;amp; maps/diagrams showing the location of rocks in the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;
Temple, R.K., Grogran, R.M.,Â &lt;span&gt;1965, C&lt;span&gt;arbonatite and related alkalic rocks at powder horn, Colorado:Â &lt;span&gt;Economic geology and the bulletin of the Society of Economic Geologists, v. 60, p.Â &lt;span&gt;672-692, doi:Â 10.2113/gsecongeo.60.4.672. &lt;a title="Full Article" href="http://dx.doi.org/10.2113/gsecongeo.60.4.672."&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Basic information regarding the structure, geochemistry, and petrogenesis of the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Van Gosen, B. S., Lowers, H. A., 2007, Iron Hill (Powderhorn)Â carbonatiteÂ complex, Gunnison County, CO; a potential source of several uncommon mineral resources: Mining Engineering, v. 59, p. 56-62, doi: N/AÂ &lt;a title="Abstract" href="http://me.smenet.org/abstract.cfm?articleID=1143&amp;amp;page=56"&gt;Abstract.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Mineral resource potential: titanium, iron, vermiculite, vanadium, and nephaline.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Olson, J.C., Hedland, D.C., &lt;span&gt;1981&lt;/span&gt;, &lt;span&gt;Alkalic rocks and resources of thorium and associated elements in the Powderhorn District, Gunnison County, Colorado&lt;/span&gt;: &lt;span&gt;USGS Numbered Series&lt;/span&gt;, Professional Paper , v. &lt;span&gt;1049, &lt;span&gt;p. C1-C34&lt;/span&gt;Â &lt;/span&gt;Â doi: N/A. &lt;a title="Full Article" href="http://pubs.usgs.gov/pp/1049c/report.pdf"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Extensive report by the USGS regarding rock type and history of formation (geologic ages).&lt;/li&gt;
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                    <text>PH-20 Hand Sample - Horizontal.</text>
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                  <text>(PH) Powderhorn (Iron Hill) Carbonatite Suite -- Gunnison County, SW Colorado</text>
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                  <text>The Powderhorn (Iron Hill) Carbonatite is located in Gunnison County in about the center of the southwestern quadrant of Colorado. It is a pear-shaped body which is essentially conical at depth, and is exposed over an area of about 12 square miles. The carbonatite body covers about 2 and a half square miles; About 70 percent of the in pyroxenite which was subsequently intruded by or replaced by nepheline and melilite-bearing rocks; magnetite-perovskite, and carbonatite.</text>
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                  <text>Western Minerals Inc.</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Mitchell, R.H., 2014, Primary and secondary niobium mineral deposits associated with carbonatites:Â Ore Geology Reviews,Â v. 64, p.Â 626-641,Â doi:10.1016/j.oregeorev.2014.03.010. &lt;a title="Full Article." href="http://dx.doi.org/10.1016/j.oregeorev.2014.03.010"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Focuses specifically on the formation of niobium in carbonatites but includes an excellent baseline description of carbonatites.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Nash, W.P., 1972, Mineralogy and Petrology of the Iron HillÂ &lt;span class="search-result-highlight"&gt;Carbonatite&lt;/span&gt;Â Complex, Colorado: Geological Society of America Bulletin, &lt;span class="cit-vol"&gt;&lt;span class="cit-sep cit-sep-before-article-vol"&gt;v.Â &lt;/span&gt;83&lt;span class="cit-sep cit-sep-after-article-vol"&gt;, p.Â &lt;/span&gt;&lt;/span&gt;&lt;span class="cit-pages"&gt;&lt;span class="cit-first-page"&gt;1361&lt;/span&gt;&lt;span class="cit-sep"&gt;-&lt;/span&gt;&lt;span class="cit-last-page"&gt;1382&lt;/span&gt;&lt;/span&gt;, doi:Â 10.1130/0016-7606(1972)83[1361:MAPOTI]2.0.CO;2. &lt;a title="Full Article." href="http://dx.doi.org/10.1130/0016-7606(1972)83%5B1361:MAPOTI%5D2.0.CO;2"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Bulk rock chemistry description &amp;amp; maps/diagrams showing the location of rocks in the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;
Temple, R.K., Grogran, R.M.,Â &lt;span&gt;1965, C&lt;span&gt;arbonatite and related alkalic rocks at powder horn, Colorado:Â &lt;span&gt;Economic geology and the bulletin of the Society of Economic Geologists, v. 60, p.Â &lt;span&gt;672-692, doi:Â 10.2113/gsecongeo.60.4.672. &lt;a title="Full Article" href="http://dx.doi.org/10.2113/gsecongeo.60.4.672."&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Basic information regarding the structure, geochemistry, and petrogenesis of the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Van Gosen, B. S., Lowers, H. A., 2007, Iron Hill (Powderhorn)Â carbonatiteÂ complex, Gunnison County, CO; a potential source of several uncommon mineral resources: Mining Engineering, v. 59, p. 56-62, doi: N/AÂ &lt;a title="Abstract" href="http://me.smenet.org/abstract.cfm?articleID=1143&amp;amp;page=56"&gt;Abstract.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Mineral resource potential: titanium, iron, vermiculite, vanadium, and nephaline.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Olson, J.C., Hedland, D.C., &lt;span&gt;1981&lt;/span&gt;, &lt;span&gt;Alkalic rocks and resources of thorium and associated elements in the Powderhorn District, Gunnison County, Colorado&lt;/span&gt;: &lt;span&gt;USGS Numbered Series&lt;/span&gt;, Professional Paper , v. &lt;span&gt;1049, &lt;span&gt;p. C1-C34&lt;/span&gt;Â &lt;/span&gt;Â doi: N/A. &lt;a title="Full Article" href="http://pubs.usgs.gov/pp/1049c/report.pdf"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Extensive report by the USGS regarding rock type and history of formation (geologic ages).&lt;/li&gt;
&lt;/ul&gt;</text>
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      <description>A physical material with a mineral composition.</description>
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          <name>Number of Thin Sections</name>
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                <text>Carbonatite </text>
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                <text>Iron rich Carbonatite.</text>
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                <text>Western Minerals Inc.</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/items/show/33"&gt;Powderhorn (Iron Hill)Carbonatite Suite-&lt;br /&gt;Gunnison County SW Colorado Collection&lt;/a&gt;</text>
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                <text>Purchased from Western Minerals Inc.</text>
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                  <text>Contains all rocks that are not part of a designated suite and have an ID number starting with R.</text>
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                  <text>Various sources</text>
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                <text>Carbonatite</text>
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                <text>Powder Horn, CO</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/1"&gt;General Rocks Suite&lt;/a&gt;</text>
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