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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>&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>Macroscopic: Staurolite, garnet, biotite porphyroblastic, chlorite bearing, muscovite schist. Both garnets and staurolite are idiomorphic with the former highly poikiloblastic. The foliation in the schist bends around the porphyroblastic phases indicating the porphyroblasts were formed earlier during metamorphism. Microscopic: Both thin section pictures show the texture of the fine grained biotite around garnet and staurolite phenocrysts. Thin section pictures in XPL unless otherwise noted in the title of the picuture. Thin sections are 3mm across.</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>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;
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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;
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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>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>&lt;strong&gt;Start Here&lt;/strong&gt;:&lt;br /&gt;Blakey, R.C., and Middleton, L.T., 2012, Geologic history and paleogeography of paleozoic and early mesozoic sedimentary rocks, eastern Grand Canyon, Arizona: Geologic Society of America Bulletin, v. 489, pp. 81-92, doi: &lt;a href="%20http%3A//dx.doi.org/10.1130/2012.2489(05)"&gt;10.1130/2012.2489(05)&lt;/a&gt;&lt;br /&gt;&lt;a href="http://dx.doi.org/10.1130/2012.2489(05)%20" target="_blank"&gt;&lt;br /&gt;&lt;/a&gt;
&lt;ul&gt;&lt;li&gt;This reference outlines the stratigraphy found in this suite. It specifically highlights the paleozoic era in which the samples represent.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional Resources:Â &lt;br /&gt;&lt;/strong&gt;Brown, E.H., Babcock, R.S., Clark, M.D., and Livingston, D.E., 1979,Â Geology of the older Precambrian rocks of the Grand Canyon Part I. Petrology and structure of the Vishnu Complex: Precambrian Research, v. 8, p. 219-241, doi:Â &lt;a href="http://dx.doi.org/10.1016/0301-9268(79)90030-5%20"&gt;10.1016/0301-9268(79)90030-5Â &lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Brown et al. begins this series of 3 articles outlining the geologic timescale and discusses the Vishnu complex and how it fits into the geologic timescale. It provides an explaination for several of the samples in this collection.Â &lt;/li&gt;
&lt;/ul&gt;
Brown, E.H., Babcock, R.S., Clark, M.D., and Livingston, D.E., 1979,Â Geology of the older Precambrian rocks of the Grand Canyon Part II. The Zoroaster Plutonic Complex and related rocks: Precambrian Research, v. 8, p. 243-275, doi&lt;span&gt;&lt;span&gt;:Â &lt;a href="http://dx.doi.org/10.1016/0301-9268(79)90031-7" target="_blank"&gt;10.1016/0301-9268(79)90031-7&lt;/a&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;In the second part of the article, the authors discuss the importance of the pluton and how it affected the formation of the stratigraphic profile of the grand canyon.Â &lt;/li&gt;
&lt;/ul&gt;
Clark, M.D., 1979,Â Geology of the older Precambrian rocks of the Grand Canyon. Part III. Petrology of mafic schists and amphibolites: Precambrian Research, v. 8, p. 277-302, doi&lt;span&gt;&lt;span&gt;:Â &lt;a href="http://dx.doi.org/10.1016/0301-9268(79)90032-9" target="_blank"&gt;10.1016/0301-9268(79)90032-9&lt;/a&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;The final section of this discussion set provides insight into the mafic layers of the stratigraphic column.Â &lt;/li&gt;
&lt;/ul&gt;
Ilg, B.R., Karlstrom, K.E., Hawkins, D.P., and Williams, M.L., 1996,Â Tectonic evolution of Paleoproterozoic rocks in the Grand Canyon: Insights into middle-crustal processes:Â Bulletin of the Geological Society of America, v. 108, p. 1149-1166, doi&lt;span&gt;&lt;span&gt;:Â &lt;a href="http://dx.doi.org/10.1130/0016-7606(1996)108" target="_blank"&gt;10.1130/0016-7606(1996)108&lt;/a&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;This is a general look into the formation of the stratigraphic layers. This article does a good job combining the above articles into one condensed summary.Â &lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>&lt;strong&gt;Start Here&lt;/strong&gt;:&lt;br /&gt;Blakey, R.C., and Middleton, L.T., 2012, Geologic history and paleogeography of paleozoic and early mesozoic sedimentary rocks, eastern Grand Canyon, Arizona: Geologic Society of America Bulletin, v. 489, pp. 81-92, doi: &lt;a href="%20http%3A//dx.doi.org/10.1130/2012.2489(05)"&gt;10.1130/2012.2489(05)&lt;/a&gt;&lt;br /&gt;&lt;a href="http://dx.doi.org/10.1130/2012.2489(05)%20" target="_blank"&gt;&lt;br /&gt;&lt;/a&gt;
&lt;ul&gt;&lt;li&gt;This reference outlines the stratigraphy found in this suite. It specifically highlights the paleozoic era in which the samples represent.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional Resources:Â &lt;br /&gt;&lt;/strong&gt;Brown, E.H., Babcock, R.S., Clark, M.D., and Livingston, D.E., 1979,Â Geology of the older Precambrian rocks of the Grand Canyon Part I. Petrology and structure of the Vishnu Complex: Precambrian Research, v. 8, p. 219-241, doi:Â &lt;a href="http://dx.doi.org/10.1016/0301-9268(79)90030-5%20"&gt;10.1016/0301-9268(79)90030-5Â &lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Brown et al. begins this series of 3 articles outlining the geologic timescale and discusses the Vishnu complex and how it fits into the geologic timescale. It provides an explaination for several of the samples in this collection.Â &lt;/li&gt;
&lt;/ul&gt;
Brown, E.H., Babcock, R.S., Clark, M.D., and Livingston, D.E., 1979,Â Geology of the older Precambrian rocks of the Grand Canyon Part II. The Zoroaster Plutonic Complex and related rocks: Precambrian Research, v. 8, p. 243-275, doi&lt;span&gt;&lt;span&gt;:Â &lt;a href="http://dx.doi.org/10.1016/0301-9268(79)90031-7" target="_blank"&gt;10.1016/0301-9268(79)90031-7&lt;/a&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;In the second part of the article, the authors discuss the importance of the pluton and how it affected the formation of the stratigraphic profile of the grand canyon.Â &lt;/li&gt;
&lt;/ul&gt;
Clark, M.D., 1979,Â Geology of the older Precambrian rocks of the Grand Canyon. Part III. Petrology of mafic schists and amphibolites: Precambrian Research, v. 8, p. 277-302, doi&lt;span&gt;&lt;span&gt;:Â &lt;a href="http://dx.doi.org/10.1016/0301-9268(79)90032-9" target="_blank"&gt;10.1016/0301-9268(79)90032-9&lt;/a&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;The final section of this discussion set provides insight into the mafic layers of the stratigraphic column.Â &lt;/li&gt;
&lt;/ul&gt;
Ilg, B.R., Karlstrom, K.E., Hawkins, D.P., and Williams, M.L., 1996,Â Tectonic evolution of Paleoproterozoic rocks in the Grand Canyon: Insights into middle-crustal processes:Â Bulletin of the Geological Society of America, v. 108, p. 1149-1166, doi&lt;span&gt;&lt;span&gt;:Â &lt;a href="http://dx.doi.org/10.1130/0016-7606(1996)108" target="_blank"&gt;10.1130/0016-7606(1996)108&lt;/a&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;This is a general look into the formation of the stratigraphic layers. This article does a good job combining the above articles into one condensed summary.Â &lt;/li&gt;
&lt;/ul&gt;</text>
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          <name>Number of Thin Sections</name>
          <description>Number of thin sections associated with this sample</description>
          <elementTextContainer>
            <elementText elementTextId="27676">
              <text>1</text>
            </elementText>
          </elementTextContainer>
        </element>
      </elementContainer>
    </itemType>
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      <elementSet elementSetId="1">
        <name>Dublin Core</name>
        <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="43">
            <name>Identifier</name>
            <description>An unambiguous reference to the resource within a given context</description>
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              <elementText elementTextId="27669">
                <text>BKM-13</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="27670">
                <text>Syenite  </text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="115">
            <name>Spatial Coverage</name>
            <description>Spatial characteristics of the resource.</description>
            <elementTextContainer>
              <elementText elementTextId="27671">
                <text>Gilford, New Hampshire</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="118">
            <name>Accrual Periodicity</name>
            <description>The frequency with which items are added to a collection.</description>
            <elementTextContainer>
              <elementText elementTextId="27672">
                <text>1980</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="37">
            <name>Contributor</name>
            <description>An entity responsible for making contributions to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="27673">
                <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="27674">
                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/df566258e339655610e57ce52cf18970.pdf"&gt;BKM Rock Suite&lt;/a&gt;</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="27675">
                <text>coarse grained</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="117">
            <name>Accrual Method</name>
            <description>The method by which items are added to a collection.</description>
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              <elementText elementTextId="27677">
                <text>Purchased from Western Minerals, Inc.</text>
              </elementText>
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          </element>
        </elementContainer>
      </elementSet>
    </elementSetContainer>
  </item>
</itemContainer>
