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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;br /&gt;&lt;/strong&gt;Cox, K.G., 1972, The Karroo Volcanic Cycle: Journal of the Geological Society, v. 128, p. 311-336.&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;Â doi: 10.1144/gsjgs. 128.4.0311.&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;The petrogenesis of the Mesozoic igneous rocks of south-Eastern Africa is related to the tectonic event believed to be the initiation of the break up of Gondwanaland. The cycle began with the rise of potassium-rich picritic magma, the source material for rocks of the northern province, Rhodesia. On top of and peripheral to the main magma body, a zone of sodic magma was generated and formed some of the rocks of the north and most southern rocks.&lt;/li&gt;
&lt;/ul&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;br /&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;White, R.S., 1992, Magmatism During and After Continental Break-Up, Geological Society, London, Special Publications, v. 68, p. 1-16. doi:Â &lt;span&gt;10.1144/GSL.SP.1992.068.01.0.&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Magmatism that goes along with continental break-up is caused primarily by decompression melting of the underlying mantle as it rises up beneath the rift. The amount of melt produced is determined by the asthenospheric mantle temperature and on the rate of rifting.Â &lt;/li&gt;
&lt;/ul&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span&gt;Eales, H.V., and van Robey, J.A., 1976, Differentiation of Tholeiitic Karroo Magma at Birds River, South Africa, Contributions to Mineralogy and Petrology 10. v. 56, p. 101-117. doi:Â &lt;span&gt;10.1007/BF00375423&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Strongly fractionated residue from the partial crystallization of tholeiitic gabbroic magma was emplaced at depth within sediment of the upper part of the Karroo succession. The residue was most likely tapped from a deeper intrusion during cauldron subsidence, but was engulfed by a later intrusion of olivine gabbro on a large scale.&lt;/li&gt;
&lt;/ul&gt;
Walker, F., and Poldervaart, A., 1949, Karroo Dolerites of the Union of South Africa, Geological Society of America Bulletin, v. 60, p. 591-706. doi: 10.1130/0016-7606(1949)60&lt;span&gt;[591:KDOTUO]2.0.CO;2&lt;/span&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;The Karroo dolerites are the result of the intrusive phase of the early Jurassic basalts that built up the Basutoland lava plateau. Most of the dolerites show little differentiation but olivine rich types and acidic veins have been recorded. The magma had an effect on the sedimentary rocks; many of the rocks described as granophyre were found to be transformed siltstone. The dolerites occur as sills and dikes but "bell-jar inclusions" occur (the Bird's River complex is a bell jar shaped inclusion).Â &lt;/li&gt;
&lt;/ul&gt;
Eales, H.V., and Booth P.W.K., 1974, The Birds River Gabbro Complex, Dordrecht District, Transactions of the Geological Society of South Africa, v. 77, p. 1-15.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;On the gabbros of the Birds River Complex.&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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