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Mysterious Midcontinent Rift is a geological hybrid. The volcanic rocks of the 1.1 billion-year-old Midcontinent Rift play a prominent role in the natural beauty of Isle Royale National Park in Lake Superior. Credit: Image courtesy of Northwestern University. An international team of geologists has a new explanation for how the Midwest’s ...Geophysical investigations and crustal structure of the North American Midcontinent Rift system (W.J. Hinze et al.). The igneous petrology and magmatic evolution of the Midcontinent rift system (K.W. Klewin, S.B. Shirey). The Midcontinent rift in the Lake Superior region with emphasis on its geodynamic evolution (W.F. Cannon).The Mid-continent rift system can be traced by the Mid-continent geophysical anomaly (MGA) from the surface exposure of the Keweenawan Supergroup in the Lake Superior basin southwest in the subsurface through Wisconsin, Minnesota, Iowa, Nebraska, and Kansas. Outcrop and well penetrations of the late rift Keweenawan sedimentary rocks reveal ... The Midcontinent Rift System (MRS; Wold and Hinze, 1982) is recognized by a significant elongate magnetic and gravity anomaly extending northeastward from south-central Kansas into the Lake Superior region and hence southeastward into the Michigan basin (Figure 45). Van Schmus and Hinze (1985) and Dickas (1984, 1986) provide excellent overviews ...Vol. 52, No. 4 | www.rmag.org 49 THE MOUNTAIN GEOLOGIST | October 2015 poSt-MiSSiSSippian tectonic evolution oF the neMaha tectonic Zone and Midcontinent riFt SySteM, Se neBraSka and n kanSaS Figure 1. Map of Precambrian features in the study area, and locations of the cross-sections used in the study (after Dicken et al., 2001Introduction. Three major Precambrian crustal elements are inferred to underlie Phanerozoic strata in the eastern midcontinent of Laurentia: (1) the Grenville Front Tectonic Zone, the latest Mesoproterozoic to earliest Neoproterozoic western boundary of the Grenville orogen; (2) the East Continent Rift System, a southerly extension of the …Dec 4, 2013 · Stein proposes a three-armed rift system, formed of the Midcontinent Rift and the two arms that split Laurentia and Amazonia. “In a lot of locations, when the continents break apart you seem to ... Sep 7, 2023 · The Midcontinent Rift system and surrounding Precambrian rocks are known to host highly significant mineral resources. Our project objectives are to increase understanding of this system through the integration of new and legacy geophysical data with geochemical and borehole data, map the lithology and structure of PreCambrian rocks, and develop an integrated 3D geologic model of the region. The Midcontinent Rift System (MRS) is a Middle Proterozoic failed rift system that stretches from eastern Lake Superior to central Kansas. Over most of its length, it is characterized by a central horst (dominated by mafic volcanic rocks) flanked by a series of clastic-filled basins that thicken towards the horst in the half-graben configurations.The Midcontinent Rift System (MRS) is a Middle Proterozoic failed rift system that stretches from eastern Lake Superior to central Kansas. Over most of its length, it is characterized by a central horst (dominated by mafic volcanic rocks) flanked by a series of clastic-filled basins that thicken towards the horst in the half-graben configurations.Mar 1, 2002 · The Midcontinent Rift System (MRS) of central North America is a 1.1-Ga, 2500-km long structural feature that has been interpreted as a triple-junction rift developed over a mantle plume. As much as 20 km of subaerial lava flows , mainly flood basalts , are overlain by as much as 10 km of sedimentary rocks that are mostly continental fluvial ... 2 The rift today. 3 Natural resources. 4 Gallery. 5 See also. 6 References. 7 External links. Toggle the table of contents Toggle the table of contents. Midcontinent Rift System. 3 languages. Français; Italiano;The 1.1 Ga Midcontinent Rift of North America is a failed intracontinental rift that was active for ∼25 m.y. Paleomagnetic and geochronologic data from Midcontinent Rift volcanic rocks have yielded a well-resolved apparent polar wander path (APWP) known as the Keweenawan Track, which records dramatic paleogeographic change throughout the life span of the rift.The Midcontinent Rift System (MRS) of North America represenThe Midcontinent Rift developed contemporaneously with northw Midcontinent Rift. The Midcontinent Rift (MCR), a 3000-km-long band of more than 2 million km 3 of buried igneous and sedimentary rocks that outcrop near Lake Superior, has been extensively studied, as reviewed by Ojakangas et al. (2001) and S. Stein et al. (2018). To the south, it is buried by younger sediments, but easily traced because the rift-filling volcanic rocks are dense and highly ... The Proterozoic Midcontinent Rift System of North Americ The North American Midcontinent Rift System (MRS) is a major magmatic continental rift that stretches approximately 2200 km from Kansas northeast to the Lake Superior region, where it curves southward and is inferred to extend into lower Michigan (Figure 1; Ojakangas et al., 2001a). The Duluth Complex (Minnesota, USA) is one of the largest mafic

Abstract: The Keweenaw fault system along Lake Superior's south shore in Michigan, USA is one of the most significant fault systems associated with North America's Midcontinent Rift System. Reverse slip has thrust Portage Lake Volcanics (ca. 1.1 Ga) southeastward over Jacobsville Sandstone (ca. 1.0 Ga).The Keweenawan Midcontinent rift system was imposed upon the terrane suture in our study area at ca. 1100 Ma. This event nearly separated the ancient continent and imparted enormous volumes of mafic magma to various depths in the crust (Hinze et al., 1997; Nicholson et al., 1997; Vervoort et al., 2007; Stein et al., 2015), engendering numerous high-grade base and precious metal deposits ...Oct 30, 2015 · Magmatic Ni-Cu-PGE mineralization in the ~ 1.1 Ga Midcontinent Rift System (Fig. 1) in North America can be broadly divided into three types (see a recent review by Ripley, 2014). Disseminated sulfide mineralization occurs within multiple, sheet-like intrusions that comprise a large portion of the Duluth Complex. Using sequential restorations of three published cross sections within Nebraska and Kansas this study demonstrates that the Nemaha Tectonic Zone and Midcontinent Rift System have each been reactivated several times since the end of the Mississippian (the details of deformation prior to the Mississippian are not considered).Midcontinent Rift System is part of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. If you would like to participate, you can choose to edit this article, or visit the project page for more information.

"The rift system is splitting Africa and rifting Arabia away from it, forming new ocean basins in the Red Sea and Gulf of Aden," explained Seth Stein, ... Detailed mapping of the underground Midcontinent Rift using gravity data from G. Randy Keller, professor of geophysics at the University of Oklahoma in Norman and director of the Oklahoma ...The Midcontinent Rift System, which curves for more than 2000 km across the Upper Midwest, is one of the world’s great continental rifts. Rifting began about 1.1 billion years ago, when the Earth’s crust ……

Reader Q&A - also see RECOMMENDED ARTICLES & FAQs. The Midcontinent Rift is an ancient rift syst. Possible cause: However, these deep cave systems can form by epigenic (top-down) processes, with meteo.