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                  <text>The suite consists of samples from an ophiolite suite that outcrops in 3 locations in the Apennine mountain range in northern Italy.Â  The units are severely imbricated and folded.Â  The units are Cretaceous-Eocene in age.Â  The units consist of ultramafic rock, gabbro and peridotite instrusions, and basaltic magmas.</text>
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                  <text>Northern Apennines, Liguria Region, Italy&lt;br /&gt;Samples 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, and 15 are taken from the region around Bargone, Italy&lt;br /&gt;Samples 14, 16, 17, 18, 19, 20, and 21 are taken from the region around Sassello, Italy&lt;br /&gt;Sample 22 is taken from outside Genoa, Italy</text>
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                  <text>Purchased by Western Minerals, Inc.</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;/strong&gt;&lt;span class="cit-auth cit-auth-type-author"&gt;Lagabrielle, Y.,&lt;/span&gt;&lt;span class="cit-sep cit-sep-two-item-separator"&gt;Â and Cannat, M., 1990, &lt;/span&gt;&lt;span class="cit-title"&gt;Alpine Jurassic ophiolites resemble the modern central Atlantic basement: Geology, v. 18, p. 319-322&lt;br /&gt;&lt;/span&gt;Link:Â &lt;a href="http://geology.geoscienceworld.org/content/18/4/319.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This fairly short article gives some insight into the development of the North Apennine Ophiolites with a fairly recent view on the matter.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;&lt;strong&gt;:&lt;/strong&gt;&lt;br /&gt;Garuti, G., and Zaccarini, F., 2005, Minerals of Au, Ag and U in Volcanic-Rock-Associated Massive Sulfide Deposits of the Northern Apennine Ophiolite, Italy: The Canadian Mineralogist, v. 43, p. 935-950&lt;br /&gt;DOI: &lt;a href="http://dx.doi.org/10.2113/gscanmin.43.3.935" target="_blank"&gt;10.2113/gscanmin.43.3.935&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the elemental composition of the North Apennine Ophiolite sequence and uses that to determine previous geologic events.&lt;/li&gt;
&lt;/ul&gt;
Garuti, G., Zaccarini, F., Scacchetti, M., and Bartoli, O., 2011, The Pb-rich sulfide veins in the Boccassuolo ophiolite: Implications for the geochemical evolution of the hydrothermal activity across the ocean-continent transition in the Ligurian Tethys (Northern-Apennine, Italy): Lithos, v. 124, p. 243-254&lt;br /&gt;DOI:Â &lt;a title="10.1016/j.lithos.2010.11.006" href="http://dx.doi.org/10.1016/j.lithos.2010.11.006" target="_blank"&gt;10.1016/j.lithos.2010.11.006&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the chemical composition of the ophiolite sequence under a different name and ties it into the formation history.&lt;/li&gt;
&lt;/ul&gt;
Garzanti, E., Canclini, S., Foggia, F.M., and Petrella, N., 2002, Unraveling Magmatic and Orogenic Provenance in Modern Sand: The Back-Arc Side of the Apennine Thrust Belt, Italy: Journal of Sedimentary Research, v. 72, p. 2-17&lt;br /&gt;DOI:Â &lt;a title="10.1306/051801720002" href="http://dx.doi.org/10.1306/051801720002" target="_blank"&gt;&lt;span&gt;10.1306/051801720002&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into great detail on the provenance characteristics for a number of sands. including sands originating from the North Apennine Ophiolite sequence.&lt;/li&gt;
&lt;/ul&gt;
Cibin, U., Spadafora, E., Zuffa, G.G., and Castellarin, A., 2001, Continental collision history from arenites of episutural basins in the Northern Apennines, Italy: Geological Society of America Bulletin, v. 113, p. 4-19&lt;br /&gt;Link: &lt;a title="GeoScienceWorld" href="http://bulletin.geoscienceworld.org/content/113/1/4.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into detail about the deformations experienced by the North Apennine Ophiolites after the Eocene.&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>Dioritic gabbro with deformational oceanic metamorphism of amphibolitic to greenschist facies and overprinting of prehnite-pumpellite.&#13;
Primary phases: plagioclase, clinopyroxene, olivine, ilmenite. Oceanic metamorphic paragenesis: plagioclase, clinopyroxene, green to dark hornblende, actinolite, tremolite, chlorite.&#13;
Prehnite-pumpellyite metamorphic paragenesis: plagioclase saussuritization with possible neoformation of pumpellyite, clinozoisite, prehnite, chlorite. Gneissic-occhiadine (augen), with development of banded structure with different composition.&#13;
Porphyroclasts of the primary phases surrounded by newly formed granoblastic aggregates; tremolite and chlorite aggregates pseudomorphs of olivine. Very fine-grained neoformation of the phases of the prehnite-pumpellyite facies.</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;
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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;
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&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;
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;/strong&gt;&lt;span class="cit-auth cit-auth-type-author"&gt;Lagabrielle, Y.,&lt;/span&gt;&lt;span class="cit-sep cit-sep-two-item-separator"&gt;Â and Cannat, M., 1990, &lt;/span&gt;&lt;span class="cit-title"&gt;Alpine Jurassic ophiolites resemble the modern central Atlantic basement: Geology, v. 18, p. 319-322&lt;br /&gt;&lt;/span&gt;Link:Â &lt;a href="http://geology.geoscienceworld.org/content/18/4/319.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This fairly short article gives some insight into the development of the North Apennine Ophiolites with a fairly recent view on the matter.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;&lt;strong&gt;:&lt;/strong&gt;&lt;br /&gt;Garuti, G., and Zaccarini, F., 2005, Minerals of Au, Ag and U in Volcanic-Rock-Associated Massive Sulfide Deposits of the Northern Apennine Ophiolite, Italy: The Canadian Mineralogist, v. 43, p. 935-950&lt;br /&gt;DOI: &lt;a href="http://dx.doi.org/10.2113/gscanmin.43.3.935" target="_blank"&gt;10.2113/gscanmin.43.3.935&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the elemental composition of the North Apennine Ophiolite sequence and uses that to determine previous geologic events.&lt;/li&gt;
&lt;/ul&gt;
Garuti, G., Zaccarini, F., Scacchetti, M., and Bartoli, O., 2011, The Pb-rich sulfide veins in the Boccassuolo ophiolite: Implications for the geochemical evolution of the hydrothermal activity across the ocean-continent transition in the Ligurian Tethys (Northern-Apennine, Italy): Lithos, v. 124, p. 243-254&lt;br /&gt;DOI:Â &lt;a title="10.1016/j.lithos.2010.11.006" href="http://dx.doi.org/10.1016/j.lithos.2010.11.006" target="_blank"&gt;10.1016/j.lithos.2010.11.006&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the chemical composition of the ophiolite sequence under a different name and ties it into the formation history.&lt;/li&gt;
&lt;/ul&gt;
Garzanti, E., Canclini, S., Foggia, F.M., and Petrella, N., 2002, Unraveling Magmatic and Orogenic Provenance in Modern Sand: The Back-Arc Side of the Apennine Thrust Belt, Italy: Journal of Sedimentary Research, v. 72, p. 2-17&lt;br /&gt;DOI:Â &lt;a title="10.1306/051801720002" href="http://dx.doi.org/10.1306/051801720002" target="_blank"&gt;&lt;span&gt;10.1306/051801720002&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into great detail on the provenance characteristics for a number of sands. including sands originating from the North Apennine Ophiolite sequence.&lt;/li&gt;
&lt;/ul&gt;
Cibin, U., Spadafora, E., Zuffa, G.G., and Castellarin, A., 2001, Continental collision history from arenites of episutural basins in the Northern Apennines, Italy: Geological Society of America Bulletin, v. 113, p. 4-19&lt;br /&gt;Link: &lt;a title="GeoScienceWorld" href="http://bulletin.geoscienceworld.org/content/113/1/4.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into detail about the deformations experienced by the North Apennine Ophiolites after the Eocene.&lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;/strong&gt;&lt;span class="cit-auth cit-auth-type-author"&gt;Lagabrielle, Y.,&lt;/span&gt;&lt;span class="cit-sep cit-sep-two-item-separator"&gt;Â and Cannat, M., 1990, &lt;/span&gt;&lt;span class="cit-title"&gt;Alpine Jurassic ophiolites resemble the modern central Atlantic basement: Geology, v. 18, p. 319-322&lt;br /&gt;&lt;/span&gt;Link:Â &lt;a href="http://geology.geoscienceworld.org/content/18/4/319.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This fairly short article gives some insight into the development of the North Apennine Ophiolites with a fairly recent view on the matter.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;&lt;strong&gt;:&lt;/strong&gt;&lt;br /&gt;Garuti, G., and Zaccarini, F., 2005, Minerals of Au, Ag and U in Volcanic-Rock-Associated Massive Sulfide Deposits of the Northern Apennine Ophiolite, Italy: The Canadian Mineralogist, v. 43, p. 935-950&lt;br /&gt;DOI: &lt;a href="http://dx.doi.org/10.2113/gscanmin.43.3.935" target="_blank"&gt;10.2113/gscanmin.43.3.935&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the elemental composition of the North Apennine Ophiolite sequence and uses that to determine previous geologic events.&lt;/li&gt;
&lt;/ul&gt;
Garuti, G., Zaccarini, F., Scacchetti, M., and Bartoli, O., 2011, The Pb-rich sulfide veins in the Boccassuolo ophiolite: Implications for the geochemical evolution of the hydrothermal activity across the ocean-continent transition in the Ligurian Tethys (Northern-Apennine, Italy): Lithos, v. 124, p. 243-254&lt;br /&gt;DOI:Â &lt;a title="10.1016/j.lithos.2010.11.006" href="http://dx.doi.org/10.1016/j.lithos.2010.11.006" target="_blank"&gt;10.1016/j.lithos.2010.11.006&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the chemical composition of the ophiolite sequence under a different name and ties it into the formation history.&lt;/li&gt;
&lt;/ul&gt;
Garzanti, E., Canclini, S., Foggia, F.M., and Petrella, N., 2002, Unraveling Magmatic and Orogenic Provenance in Modern Sand: The Back-Arc Side of the Apennine Thrust Belt, Italy: Journal of Sedimentary Research, v. 72, p. 2-17&lt;br /&gt;DOI:Â &lt;a title="10.1306/051801720002" href="http://dx.doi.org/10.1306/051801720002" target="_blank"&gt;&lt;span&gt;10.1306/051801720002&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into great detail on the provenance characteristics for a number of sands. including sands originating from the North Apennine Ophiolite sequence.&lt;/li&gt;
&lt;/ul&gt;
Cibin, U., Spadafora, E., Zuffa, G.G., and Castellarin, A., 2001, Continental collision history from arenites of episutural basins in the Northern Apennines, Italy: Geological Society of America Bulletin, v. 113, p. 4-19&lt;br /&gt;Link: &lt;a title="GeoScienceWorld" href="http://bulletin.geoscienceworld.org/content/113/1/4.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into detail about the deformations experienced by the North Apennine Ophiolites after the Eocene.&lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>The suite consists of samples from an ophiolite suite that outcrops in 3 locations in the Apennine mountain range in northern Italy.Â  The units are severely imbricated and folded.Â  The units are Cretaceous-Eocene in age.Â  The units consist of ultramafic rock, gabbro and peridotite instrusions, and basaltic magmas.</text>
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                  <text>Northern Apennines, Liguria Region, Italy&lt;br /&gt;Samples 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, and 15 are taken from the region around Bargone, Italy&lt;br /&gt;Samples 14, 16, 17, 18, 19, 20, and 21 are taken from the region around Sassello, Italy&lt;br /&gt;Sample 22 is taken from outside Genoa, Italy</text>
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                  <text>Purchased by Western Minerals, Inc.</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;/strong&gt;&lt;span class="cit-auth cit-auth-type-author"&gt;Lagabrielle, Y.,&lt;/span&gt;&lt;span class="cit-sep cit-sep-two-item-separator"&gt;Â and Cannat, M., 1990, &lt;/span&gt;&lt;span class="cit-title"&gt;Alpine Jurassic ophiolites resemble the modern central Atlantic basement: Geology, v. 18, p. 319-322&lt;br /&gt;&lt;/span&gt;Link:Â &lt;a href="http://geology.geoscienceworld.org/content/18/4/319.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This fairly short article gives some insight into the development of the North Apennine Ophiolites with a fairly recent view on the matter.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;&lt;strong&gt;:&lt;/strong&gt;&lt;br /&gt;Garuti, G., and Zaccarini, F., 2005, Minerals of Au, Ag and U in Volcanic-Rock-Associated Massive Sulfide Deposits of the Northern Apennine Ophiolite, Italy: The Canadian Mineralogist, v. 43, p. 935-950&lt;br /&gt;DOI: &lt;a href="http://dx.doi.org/10.2113/gscanmin.43.3.935" target="_blank"&gt;10.2113/gscanmin.43.3.935&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the elemental composition of the North Apennine Ophiolite sequence and uses that to determine previous geologic events.&lt;/li&gt;
&lt;/ul&gt;
Garuti, G., Zaccarini, F., Scacchetti, M., and Bartoli, O., 2011, The Pb-rich sulfide veins in the Boccassuolo ophiolite: Implications for the geochemical evolution of the hydrothermal activity across the ocean-continent transition in the Ligurian Tethys (Northern-Apennine, Italy): Lithos, v. 124, p. 243-254&lt;br /&gt;DOI:Â &lt;a title="10.1016/j.lithos.2010.11.006" href="http://dx.doi.org/10.1016/j.lithos.2010.11.006" target="_blank"&gt;10.1016/j.lithos.2010.11.006&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the chemical composition of the ophiolite sequence under a different name and ties it into the formation history.&lt;/li&gt;
&lt;/ul&gt;
Garzanti, E., Canclini, S., Foggia, F.M., and Petrella, N., 2002, Unraveling Magmatic and Orogenic Provenance in Modern Sand: The Back-Arc Side of the Apennine Thrust Belt, Italy: Journal of Sedimentary Research, v. 72, p. 2-17&lt;br /&gt;DOI:Â &lt;a title="10.1306/051801720002" href="http://dx.doi.org/10.1306/051801720002" target="_blank"&gt;&lt;span&gt;10.1306/051801720002&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into great detail on the provenance characteristics for a number of sands. including sands originating from the North Apennine Ophiolite sequence.&lt;/li&gt;
&lt;/ul&gt;
Cibin, U., Spadafora, E., Zuffa, G.G., and Castellarin, A., 2001, Continental collision history from arenites of episutural basins in the Northern Apennines, Italy: Geological Society of America Bulletin, v. 113, p. 4-19&lt;br /&gt;Link: &lt;a title="GeoScienceWorld" href="http://bulletin.geoscienceworld.org/content/113/1/4.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into detail about the deformations experienced by the North Apennine Ophiolites after the Eocene.&lt;/li&gt;
&lt;/ul&gt;</text>
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