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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>&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>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>A sampling of the four plutonic stages of the New Hampshire series. This encompasses the Bethlehem Gneiss, the Kinsman Quartz Monzonite, the Spaulding Quartz Diorite and the Concord Granite.  The rocks cover the Mascoma, Sunapee, Mt. Kearsarge, Penacook, Hillsboro, and Concord Quadrangles.  The ages of the series range from 359-411 Ma.</text>
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                  <text>&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Dorais, M.J., 2003, The petrogenesis and emplacement of the New Hampshire Plutonic Suite: American Journal of Science, v. 303, pp. 447-487,Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of each of the four series in the New Hampshire magma series.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;/strong&gt;Clark, R.G., and Lyons, J.B., 1986, Petrogenesis of the Kinsman intrusive suite; peraluminous granitiods of western New Hampshire: Journal of Petrology, v. 27, pp. 1365-1393&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of the Kinsman Quartz Monzonite in detail.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Duke, E.F., 1978, Petrology of Spaulding Group tonalites from Penacook Quadrangle, New Hampshire [Ph.D. Thesis], Dartmouth College, 117 p.Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This thesis details the emplacement, formation, and petrology of the Spaulding Quartz Diorite.&lt;/li&gt;
&lt;/ul&gt;
Lathrop, A.S., Blum, J.D., and Chamberlain, C.P., 1996, Nd, Sr and O isotopic study of the petrogeneseis of two syntectonic members of the New Hampshire plutonic series: Contributions to Mineralogy and Petrology, v. 124, pp. 126-138.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the elemental and isotopic analyses of the New Hampshire magma series in order to better understand the petrogenesis of the suite.&lt;/li&gt;
&lt;/ul&gt;
Lyons, J.B., and Livingston, D.E., 1977, Rb-Sr age of the New Hampshire Plutonic Series: Geological Society of America Bulletin, v. 88, pp. 1808-1812&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper uses Rb-Sr isotopic analyses in order to age date the four different members of the New Hampshire magma series.&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>Plutonic Magma Series- Southwestern New Hampshire: Western Minerals Supplementary Information</text>
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                <text>Lyons, J.B., and Livingston, D.E., 1977, Rb-Sr age of the New Hampshire Plutonic Series; G.S.A. Bull. v 88, p. 1808-12.</text>
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                <text>Southwestern New Hampshire. within the Mascoma Sunapee, Mt. Kearsarge, Penacook, Hillsboro and Concord quadrangles.</text>
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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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              <name>References</name>
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                <elementText elementTextId="17991">
                  <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>Purchased from Western Minerals Inc. </text>
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                  <text>These 31 samples comprise a collection of volcanic rocks associated with the hot-spot volcanism of the Hawaiian Islands. Samples were collected from various locations across the islands of Hawaii and Oahu. The collection contains samples of primarily tholeiitic &amp; alkalic basalts, pumice, scoria, oceanite, and hawaiite. </text>
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                  <text>Samples were collected from various locations on the islands of Hawaii and Oahu. </text>
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                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Macdonald, G.A., 1949, Petrography of the Island of Hawaii, U.S.G.S. Prof. Paper 214 D&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article is a part of the general investigation of the island of Hawaii by the United States Geologic Survey. The paper describes the dominant volcanoes of the island of Hawaii (from which most of the suite's samples were collected) and describes the petrographic phenomena observed and geochemical analyses of volcanic rocks.Â &lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional Resources:&lt;/strong&gt;&lt;br /&gt;Ho, R.A., Garcia, M.O., 1988, Origin of differentiated lavas at Kilauea Volcano, Hawaii; implications from the 1955 eruption: Bulletin of Volcanology, v. 50, p. 35-46.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article describes a study of lava flows from the 1955 eruption of the Kilauea Volcano on the island of Hawaii to evaluate models of crystal fractionation or magma mixing as the processes forming differentiated magmas. Through geochemical analyses, the study concluded that crystal fractionation resulted in the observed differentiation of lavas.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;br /&gt;Hofman, A.W., Farnetani, C.G., 2013, Two Views of Hawaiian Plume Structure: Geochemistry, Geophysics, Geosystems, v.14, p. 5308-5322, doi:10.1002/2013GC004942&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article presents two opposing views of the source of magmas for the Hawaiian volcanoes. Both views favor a deep mantle source, but try to explain differences in isotopic compositions.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;br /&gt;Macdonald, G.A., 1968, Composition and origin of Hawaiian LavasÂ &lt;em&gt;in&lt;/em&gt; GSA Memoirs 1968, p. 477-522&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article provides geochemical analysis of major elements as well as determinations of minor elements of volcanic rocks from the island of Hawaii. The article describes the three major rock types - tholeitic, alkalic, and nephelinic - and concludes these rock suites are chemically intergradational and are likely derived from crystal differentiation of a single parent magma.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;br /&gt;Moore, J.G., Clague, D.A., 1992, Volcano growth and evolution of the Island of Hawaii: Geologic Society of America Bulletin, v. 104, p. 1471-1484&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article proposes a chronologic evolution of the island of Hawaii, from where many of the suite's samples were collected.&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>Volcanic Phenomena Suite - The Hawiian Islands of Hawaii and Oahu, Western Minerals Supplementary Information</text>
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                <text>January 20, 1969</text>
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                  <text>(NS) Meta-Pelite Suite -- Shelburne, Nova Scotia</text>
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                  <text>Samples from the Shelburne area representative of the full range of metamorphic grades. This suite includes a high grade pelitic xenolith as well as samples of the Shelburne granite and aluminum-rich pegmatites. Furthermore a lampophric dyke that intruded from the basement rock to the Meguma Terrace is featured.</text>
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                  <text>Western Minerals, Inc.</text>
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                  <text>Purchased from Western Minerals, Inc.</text>
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                  <text>&lt;strong&gt;Start Here&lt;/strong&gt;: &lt;br /&gt;Currie, K.L., Whalen, J.B., Davis, W.J., Longstaffe, F.J., and Cousens, B.L., 1998, Geochemical evolution of peraluminous plutons in southern Nova Scotia, Canada-a pegmatite-poor suite:Lithos, v. 44, p.117-140, doi:&lt;a href="http://dx.doi.org/10.1016/S0024-4937(98)0051-6"&gt;10.1016/S0024-4937(98)0051-6&lt;/a&gt; â€¢ This paper gives information on the geology of southern Nova Scotia and provides a strong example for the rock suite present. &lt;strong&gt;&lt;br /&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;: &lt;br /&gt;&lt;br /&gt;Cambell, D., Shimeld, J., Deptuck, M.E., Mosher, J.C., Seismic Stratigraphic framework and depositional history of a large Upper Cretaceous and Cenozoic depocenter off southwest Nova Scotia, Canada: Marine and Petroleum Geology, v. 65, p. 22-42, doi: &lt;a href="http://dx.doi.org/10.1016/j.marpetgeo.2015.03.016"&gt;&lt;span class="paddingR15"&gt;&lt;span&gt;10.1016/j.marpetgeo.2015.03.016&lt;/span&gt;&lt;/span&gt;&lt;/a&gt;Â  &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful as it outlines the stratrigraphy and depositional history of the region. This is key in understanding much of the regions history and allows geologists to better understand what exactly is metamorphosed and why.&lt;br /&gt;&lt;br /&gt;Greenough, J.D., Jone, M.L., and Mossman, D.J., 1989, The Sr isotopic composition of early Jurassic mafic rocks of Atlantic Canada: Implications for assimilation and injection mechanism affecting mafic dykes: Chemical Geology, v. 80, p. 17-26, doi: &lt;a href="http://dx.doi/org/10.1016/0168-9622(89)90044-4"&gt;10.1016/0168-9622(89)90044-4&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful for describing the dykes in Atlantic Canada as well as injections that formed much of the suite. &lt;br /&gt;&lt;br /&gt;Merle, R., Marzoli, A., Reisberg, L., Bertrand, H., Nemchin, A., Chiaradia, M., Callegaro, S., Jourdan, F., Bellieni, G., Kontak, D., Puffer, J., Mchone, J., 2014, Sr, Nd, Pb, and Os isotope systematics of CAMP tholeiites from Eastern North America (ENA): Evidence of a subduction-enriched mantle source: Journal of Petrology, v. 55, p. 133-180, doi: &lt;a href="http://dx.doi.org/10.1093/petrology/egt063"&gt;&lt;span class="paddingR15"&gt;&lt;span&gt;10.1093/petrology/egt063&lt;/span&gt;&lt;/span&gt;&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper outline the subduction in the region as well as outling the petrologic controls on the region, specifically with an eye on Seldon, Nova Soctia. this is particularly imporant when considering the pegmatites in the suite and other igneous bodies.&lt;br /&gt;&lt;br /&gt;Muecke, G. K., Pride, C., and Sarkar, P., 1979, Rare-earth element geochemistry of regional metamorphic rocks: Physics and Chemistry of the Earth, v. 11, p. 449-464, doi:&lt;a href="http://dx.doi.org/10.1016/0079-1946(79)90043-0"&gt;10.1016/0079-1946(79)90043-0&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful for as it describes the geochemistry of the suite on a large scale and provides reference for what should be seen in the suite.</text>
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                  <text>Samples are Cambrian to lower Ordovician greywackes and shales that were regionally metamorphosed and intruded by granites during the Devonian. &#13;
Samples taken in 1988. </text>
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                  <text>These samples were taken from the Shelburne area of Nova Scotia. This is the southeastern shore of Nova Scotia. </text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/items/browse/1?search=&amp;amp;advanced%5B0%5D%5Belement_id%5D=&amp;amp;advanced%5B0%5D%5Btype%5D=&amp;amp;advanced%5B0%5D%5Bterms%5D=&amp;amp;range=&amp;amp;public=&amp;amp;featured=&amp;amp;collection=14&amp;amp;type=15&amp;amp;user=&amp;amp;tags=&amp;amp;geolocation-address=&amp;amp;geolocation-latitude=&amp;amp;geolocation-longitude=&amp;amp;geolocation-radius=10&amp;amp;exhibit=&amp;amp;submit_search=Search+%E2%86%92"&gt;Pelitic Metamorphic Suite Rocks&lt;/a&gt;</text>
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                <text>1988</text>
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                  <text>(TMJ) Quartz-rich Metamorphic Suite -- Tanzawa Mountains, Kanto, Japan</text>
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                  <text>The Tanzawa Mountains in Japan were created in an arc-arc collision, when the Izu-Bonin-Mariana Arc was subducted beneath the Honshu Arc. This eventually  accreted into the Tanzawa Mountains.  The samples in this collection were found in and around the Tanzawa Mountains.  The suite includes hornfels, amphibolites, quartz diorite, granophyres, and other basaltic rocks.  The samples range from fine to coarse grained.  An interesting feature found on many of the samples was a flow-like swirl of minerals in the thin section, visible in XPL.  The quartz diorite  samples had crystalline, powdery substances on them, which were analyzed using a Scanning Electron Microscope (SEM). The chemical compositions of the mentioned powdery substances were calcium, aluminum, silicon, and oxygen. </text>
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              <description>A related resource that is referenced, cited, or otherwise pointed to by the described resource.</description>
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                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Kawate, S., and Makoto, A., 1998, Petrogenesis of the Tanzawa plutonic complex, central Japan; exposed felsic middle crust of the Izu-Bonin-Mariana Arc: Island Arc, v. 7, p. 342-358, &lt;br /&gt;link: http://dx.doi.org/10.1111/j.1440-1738.1998.00194.x.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper explains the chemical variation and high SiO&lt;sub&gt;2Â &lt;/sub&gt;percentage of rocks within Tanzawa region, and describes in some depth the tectonic events that uplifted the Tanzawa Mountains. Â &lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;Kitamura, K., Ishikawa, M., and Arima, M., 2003, Petrological model of the northern Izu-Bonin-Mariana Arc crust; constraints from high-pressure measurements of elastic wave velocities of the Tanzawa plutonic rocks, central Japan: Tectonophysics, v. 371, p.213-221,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1016/S0040-1951(03)00229-4&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper researchs the variations in acoustic impedance between different hornblende-gabbroic rocks from Tanzawa, Japan.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Mikami, K., 1953, Metamorphic rocks in the southeastern margin of the Tanzawa quartz-diorite mass: Science Reports of Yokohama National University, v. 2, p. 34-49&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper studies the chemical analysis of amphibolites resulting from contact metamorphism of the quartz-diorite mass in the Tanzawa Mountains.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Tani, K., Dunkley, D. J., Kimura, J., Wysoczanski, R.J., Yamada, K., and Tatsumi, Y.,2010,Â Syncollisional rapid granitic magma formation in an arc-arc collision zone: Evidence from the Tanzawa plutonic complex, Japan:Â Geology [Boulder], v. 38, p.215-218,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1130/G30526.1&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper discusses the collison that exposed the gabbroic rocks of the Tanzawa plutonic complex, and overall gives the reader an in-depth sturctural history of the Tanzawa Mountains.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Yoshimura, T., 1997, Ca-Al silicates in low-grade metavolcanic rocks from southern Tanzawa Mountains, Central Japan: Journal of Mineralogy Petrology and Economic Geology, Â v. 92, p. 363-378, &lt;br /&gt;link: http://dx.doi.org/10.2465/ganko.92.363.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper explains prevalence of greenschist facies within the Tanzawa Mountain region, and gives the mineral composition of rocks from southern region of Tanzawa Mountains.&lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;&lt;br /&gt;&lt;br /&gt;&lt;/p&gt;</text>
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                  <text>The samples were found in the Tanzawa Mountains of Kanto, Japan. &#13;
</text>
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                  <text>The Tanzawa Mountains were formed during the late Pliocene. </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;/strong&gt;: &lt;br /&gt;Currie, K.L., Whalen, J.B., Davis, W.J., Longstaffe, F.J., and Cousens, B.L., 1998, Geochemical evolution of peraluminous plutons in southern Nova Scotia, Canada-a pegmatite-poor suite:Lithos, v. 44, p.117-140, doi:&lt;a href="http://dx.doi.org/10.1016/S0024-4937(98)0051-6"&gt;10.1016/S0024-4937(98)0051-6&lt;/a&gt; â€¢ This paper gives information on the geology of southern Nova Scotia and provides a strong example for the rock suite present. &lt;strong&gt;&lt;br /&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;: &lt;br /&gt;&lt;br /&gt;Cambell, D., Shimeld, J., Deptuck, M.E., Mosher, J.C., Seismic Stratigraphic framework and depositional history of a large Upper Cretaceous and Cenozoic depocenter off southwest Nova Scotia, Canada: Marine and Petroleum Geology, v. 65, p. 22-42, doi: &lt;a href="http://dx.doi.org/10.1016/j.marpetgeo.2015.03.016"&gt;&lt;span class="paddingR15"&gt;&lt;span&gt;10.1016/j.marpetgeo.2015.03.016&lt;/span&gt;&lt;/span&gt;&lt;/a&gt;Â  &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful as it outlines the stratrigraphy and depositional history of the region. This is key in understanding much of the regions history and allows geologists to better understand what exactly is metamorphosed and why.&lt;br /&gt;&lt;br /&gt;Greenough, J.D., Jone, M.L., and Mossman, D.J., 1989, The Sr isotopic composition of early Jurassic mafic rocks of Atlantic Canada: Implications for assimilation and injection mechanism affecting mafic dykes: Chemical Geology, v. 80, p. 17-26, doi: &lt;a href="http://dx.doi/org/10.1016/0168-9622(89)90044-4"&gt;10.1016/0168-9622(89)90044-4&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful for describing the dykes in Atlantic Canada as well as injections that formed much of the suite. &lt;br /&gt;&lt;br /&gt;Merle, R., Marzoli, A., Reisberg, L., Bertrand, H., Nemchin, A., Chiaradia, M., Callegaro, S., Jourdan, F., Bellieni, G., Kontak, D., Puffer, J., Mchone, J., 2014, Sr, Nd, Pb, and Os isotope systematics of CAMP tholeiites from Eastern North America (ENA): Evidence of a subduction-enriched mantle source: Journal of Petrology, v. 55, p. 133-180, doi: &lt;a href="http://dx.doi.org/10.1093/petrology/egt063"&gt;&lt;span class="paddingR15"&gt;&lt;span&gt;10.1093/petrology/egt063&lt;/span&gt;&lt;/span&gt;&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper outline the subduction in the region as well as outling the petrologic controls on the region, specifically with an eye on Seldon, Nova Soctia. this is particularly imporant when considering the pegmatites in the suite and other igneous bodies.&lt;br /&gt;&lt;br /&gt;Muecke, G. K., Pride, C., and Sarkar, P., 1979, Rare-earth element geochemistry of regional metamorphic rocks: Physics and Chemistry of the Earth, v. 11, p. 449-464, doi:&lt;a href="http://dx.doi.org/10.1016/0079-1946(79)90043-0"&gt;10.1016/0079-1946(79)90043-0&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful for as it describes the geochemistry of the suite on a large scale and provides reference for what should be seen in the suite.</text>
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                  <text>Samples are Cambrian to lower Ordovician greywackes and shales that were regionally metamorphosed and intruded by granites during the Devonian. &#13;
Samples taken in 1988. </text>
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        <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="15053">
                <text>Argillite with spessartine garnet</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="15054">
                <text>Macroscopic: Argillite bearing spessartine garnet formed through reaction with the surrounding rock during metamorphism. Microscopic: Abundant medium-sized garnet phenocrysts within a very fine grained matrix. Thin section pictures in XPL unless otherwise noted i the picture title. Thin sections are 3mm across.</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="40">
            <name>Date</name>
            <description>A point or period of time associated with an event in the lifecycle of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="15055">
                <text>N/A</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="37">
            <name>Contributor</name>
            <description>An entity responsible for making contributions to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="15056">
                <text>Western Minerals, Inc.</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="104">
            <name>Is Part Of</name>
            <description>A related resource in which the described resource is physically or logically included.</description>
            <elementTextContainer>
              <elementText elementTextId="15057">
                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/14"&gt;Pelitic Metamorphic Suite, Shelburne, Nova Scotia&lt;/a&gt;</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="43">
            <name>Identifier</name>
            <description>An unambiguous reference to the resource within a given context</description>
            <elementTextContainer>
              <elementText elementTextId="15058">
                <text>NS-3</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="115">
            <name>Spatial Coverage</name>
            <description>Spatial characteristics of the resource.</description>
            <elementTextContainer>
              <elementText elementTextId="15059">
                <text>Nova Scotia</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="116">
            <name>Temporal Coverage</name>
            <description>Temporal characteristics of the resource.</description>
            <elementTextContainer>
              <elementText elementTextId="15060">
                <text>N/A</text>
              </elementText>
            </elementTextContainer>
          </element>
        </elementContainer>
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