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                    <text>DUCO-11 hand sample of kyanite biotite garnet schist</text>
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                  <text>(DUCO) Barrovian Metamorphic Sequence -- Dutchess County, New York</text>
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                  <text>Western Minerals, Inc.</text>
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                  <text>A classic example of Barrovian-type metamorphism in Dutchess County, NY associated with the Taconic orogeny. A Barrovian metamorphic sequence displays gradual pressure and temperature increase along the metamorphic gradient, and occurs during regional metamorphism. These zones of pressure and temperature increase are recognizable by the characteristic minerals that accompany them. Dutchess County, NY contains an unusually complete sequence.&#13;
&#13;
This collection contains metamorphic rocks from chlorite grade to sillimanite grade in a tight spatial window which records the regional metamorphic gradient increasing  from WNW to ESE. This collection also contains some rocks that mirror the protoliths of the schists and quartzites of the sequence (shales and graywacke). </text>
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                  <text>Dutchess County, New York</text>
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                  <text>450-430 Ma</text>
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                  <text>&lt;strong&gt;Start Here:&lt;/strong&gt; &lt;br /&gt;Vollmer, F. W., and Walker, J., 2009, The classic Barrovian metamorphic sequence of Dutchess County and its structural and stratigraphic context in the Taconic Orogeny. In Guidebookâ€”New York State Geological Association Meeting, v. 81, p. 11-1.Â &lt;br /&gt;&lt;a href="http://www2.newpaltz.edu/~vollmerf/papers/Vollmer_and_Walker_2009_NYSGA.pdf"&gt;http://www2.newpaltz.edu/~vollmerf/papers/Vollmer_and_Walker_2009_NYSGA.pdf&lt;/a&gt;Â (accessed March 15th, 2015)&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;A useful field trip guide across the Barrovian metamorphic sequence of Dutchess county. Good general introduction to the geology of the area.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;/strong&gt;&lt;br /&gt;Whitney, D.L., Mechum, T.A., Keuhner, S.M., and Dilek, Y.R., 1996, Progressive metamorphism of pelitic rocks from protolith to granulite facies, Dutchess County, New York, USA: constraints on the timing of fluid infiltration during regional metamorphism, Journal of Metamorphic Geology, v. 14, p. 163-181. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.1046/j.1525-1314.1996.05836.x&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;A fairly general look at the progressive metamorphism in Dutchess County by one of the foremost workers in the area.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Knopf, E.B., 1927, Some recent work in the Taconic area: American Journal of Science, v. 41, p. 42-458. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.2475/ajs.s5-14.84.429&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;One of the first articles to describle the Dutchess County rocks as a "classic" Barrovian sequence.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Ghent, E.D., Stout, M.Z., 1981, Geobarometry and geothermometry of plagioclase-biotite-garnet-muscovite assemblages, Contributions to Mineralogy and Petrology, v. 76, p. 92-97. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.1007/BF00373688&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Work constraining the pressure and temperature paths of metamorphism in the sequence through equilibrium assemblages. This work was found to be in agreement with other equilibrium assemblage PT paths.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Whitney, D.L., Mechum, T.A., Dilek, Y.R., and Keuhner, S.M., 1996, Modification of garnet during regional metamorphism in garnet through sillimanite-zone rocks, Dutchess County, New York, American Mineralogist, v. 81, p. 696-705. &lt;a href="http://www.minsocam.org/MSA/AmMin/TOC/Articles_Free/1996/Whitney_p696-705_96.pdf"&gt; http://www.minsocam.org/MSA/AmMin/TOC/Articles_Free/1996/Whitney_p696-705_96.pdf&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Work by Whitney on changes in PTX conditions leading to modification of garnet in the metamorphic sequence. Garnet is widely distributed through the sequence, which makes it a useful marker for tracking these changes.&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>Kyanite biotite garnet schist</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/18"&gt;Barrovian Metamorphic Sequence--Dutchess County, New York&lt;/a&gt;</text>
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                <text>Schist with coarse biotite controlling foliation. Garnets visible in some hand samples. Kyanite blades without preferred orientation--at higher concentration within folds. Possibly from the Walloomsac schist.&#13;
&#13;
The PPL thin section shows biotite, muscovite, kyanite, and staurolite.&#13;
&#13;
This rock is from the kyanite zone of the Barrovian metamorphic sequence (high metamorphism). </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>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;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>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>&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>Leucocratic biotite-silimanite gneiss</text>
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                <text>Macroscopic: Leucocratic biotite, muscovite, sillimanite gneiss. A banded gneiss characterized by leucocratic minerals. Microscopic: thin section shows an abundance of muscovite and quartz. Thin section pictures in XPL unless otherwise noted in the title of the picuture. Thin sections are 3mm across.&lt;br /&gt;&lt;br /&gt;Leucocratic: Having a light color</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/14"&gt;Pelitic Metamorphic Suite, Shelburne, Nova Scotia&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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                  <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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              <description>An alternative name for the resource. The distinction between titles and alternative titles is application-specific.</description>
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                  <text>Typical turbidite sequence rocks (predominantly clastics with some evidence of carbonate input) </text>
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              <description>Spatial characteristics of the resource.</description>
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                  <text>Molasse Basin, Sternenberg, Germany</text>
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              <description>Temporal characteristics of the resource.</description>
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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>1:24000</text>
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                <text>&lt;a href="https://www.sciencebase.gov/catalog/item/5892146ee4b072a7ac13049d" target="_blank"&gt;Digital Map Link&lt;/a&gt;</text>
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            <description>A related resource</description>
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                <text>Lake Mcdonald East, Mount Jackson, Mount Stimson, Rising Sun, Mount Cannon, Many Glacier, Ahern pass, Lake Sherburne</text>
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                <text>GSCI 121, Our Geological Environment Lab (Glaciers)</text>
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