Midcontinent rift system

Magmatic Ni-Cu-PGE mineralization in the ~ 1.1 Ga M

But the 2000 km long Midcontinent Rift System is an extraordinary example of plate tectonic processes, and it spans half a dozen states in the Midwest! Most of it is concealed by deposits that have accumulated over the past 1.1 billion years, so much of what we know about the rift comes from geophysics, which is giving exciting new insights ...The Fracture Pattern of North-central Kansas and Its Relation to Hydrogen Soil Gas Anomalies Over the Midcontinent Rift System Volume 88, Issue 25 of Open-file report: Authors: Kansas Geological Survey, Scott Kenneth Johnsgard: Publisher: University of Kansas, Geology, 1988: Length: 112 pages : Export Citation: BiBTeX EndNote RefManMay 1, 1985 · North America's failed 1.1 Ga Midcontinent Rift (MCR) is one of the best preserved intra-continental rift systems of late Mesoproterozoic age (Wold and Hinze, 1982;Green, 1983; Van Schmus and ...

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Abstract and Figures. This chapter discusses the Midcontinent Rift system (MCR). The majority of the rift's igneous rocks are derived from a melting mantle plume and the overlying lithosphere over ...J. B. Paces and J. D. Miller, Jr., "Precise U-Pb Ages of Duluth Complex and Related Mafic Intrusions, Northeastern Minnesota: Geochronological Insights to Physical, Petrogenetic, Paleomagnetic, and Tectonomagmatic Processes Associated with the 1.1 Ga Midcontinent Rift System," J. Geophys. Res. 98, 997-14013 (1993).The Mesoproterozoic Midcontinent Rift System (MRS) of North America hosts a diverse suite of magmatic and hydrothermal mineral deposits in the Lake …The Midcontinent rift system is a 1.1-b.y.-old structure extending from Kansas, through the Lake Superior region, and into southern Michigan. The rift is filled with thick sequences of basaltic volcanic rocks and clastic sediments. For most of its extent it is buried beneath Paleozoic rocks but can be traced by its strong gravity and magnetic anomalies.J. B. Paces and J. D. Miller, Jr., "Precise U-Pb Ages of Duluth Complex and Related Mafic Intrusions, Northeastern Minnesota: Geochronological Insights to Physical, Petrogenetic, Paleomagnetic, and Tectonomagmatic Processes Associated with the 1.1 Ga Midcontinent Rift System," J. Geophys. Res. 98, 997-14013 (1993).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 …About 1.1 billion years ago during the Proterozoic Eon a great plume of hot mantle rock rose under this area, stretching the crust and erupting many huge basaltic lava flows (black) in the subsiding basin along the Midcontinent Rift System. Note the Earth's curvature for scale. Lake Superior would eventually form along this ancient rift system.Halls, 1997; Riller et al., 1999). Recently, the Midcontinent rift system has been interpreted as the failed arm of a triple junction as seafloor spread-ing between Laurentia and Amazonia was established (Stein et al., 2015, 2016). The volume of magmatism appears to require mantle hotspot input beyond passive rifting (Stein et al., 2015, 2016).Mid-Continent Rift Story Map By Communications and Publishing. Original Thumbnail Medium. Detailed Description. Meet the Mid-Continent Rift, one of the most geologically fascinating regions in the United States and Canada. Sources/Usage. Public Domain. Public Domain. Explore Search. Minerals; Geology; minerals; Mid-Continent;Detailed Description. The Midcontinent rift system cuts across terranes ranging in age from 3.6 to 1.65 Ga. The location of the rift south of Lake Superior in Minnesota, …Aug 4, 2016 · Called the Midcontinent Rift (MCR), this 3000-kilometer-long feature, made of 1.1-billion-year-old igneous and sedimentary rocks, extends underground across the central United States. It stands... The Midcontinent Rift developed contemporaneously with northwest-directed crustal-scale thrusting in the Grenville orogenic belt. The belt is exposed principally along the southeastern margin of the Canadian Shield, but inliers occur in the Appalachians, the East Greenland Caledonides, Texas, and Mexico. It has been traced at depth… Read More The Proterozoic Midcontinent Rift System of North America is remarkably similar to Phanerozoic rifted continental margins and flood basalt provinces. Like the younger analogues, the volcanism within this older rift can be explained by decompression melting and rapid extrusion of igneous material during lithospheric extension above a broad ...Previous Cu isotope work has documented a clear disparity between δ65Cu values of sheet-style (–0.5 to 0.5‰) and conduit-style (0.5–2.0‰) intrusions associated with the Midcontinent Rift ...The most prominent of these rifts in terms of extent and effect upon the crust is the Midcontinent Rift system (MCR) which extends in a series of generally linear segments in an arcuate pattern for a distance of over 2000 km from southern Kansas to the Lake Superior basin and then south across Michigan. The rift may also extend southerly from ...The Midcontinent Rift is an ancient rift system that could have split the country into two parts a billion years ago. In this live interview at the Sheldon Concert Hall in St. Louis, geologist Michael Wysession discusses how seismologists are using data from earthquakes and gravity measurements to characterize this underground geological scar.The U.S. Department of Energy's Office of Scientific and Technical InformationThe 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 red ...The Hranice Abyss (Czech Republic), with a reached depth of 473.5 m, is the deepest mapped extent of such a system globally, although its maximum depth is unknown. Multiple geophysical data sets (gravity, electrical resistivity tomography, audiomagnetotellurics, and seismic refraction and reflection) are used to investigate the extent and ...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 red …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 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 …Midcontinent Rift. The Midcontinent Rift (MCR), a 3The Midcontinent Rift System. Figure 2. Generalized The Midcontinent Rift System (MRS), a 2,700 km long, horseshoe shaped, intra-continental, thermo-tectonic structure of Middle Proterozoic age, extends from central Kansas to at least southern Ohio by way of the Lake Superior basin. Its western arm, geophysically identified as the Midcontinent Gravity High, has recently been clarified ...The Midcontinent Rift (MCR) of the north-central United States serves as a testing ground for this approach, where the coincidence of high gravity, low seismic velocity, and minimal topographic relief present a challenge to the generation of a viable crustal and upper mantle density model. ... F is a system of zero-order Kelvin-Bessel functions ... [Show full abstract] northeastern Kansas is a The Midcontinent rift system is a 1.1-b.y.-old structure extending from Kansas, through the Lake Superior region, and into southern Michigan. The rift is filled with thick sequences of basaltic ...@article{osti_6431485, title = {Organic Geochemical and tectonic evolution of the Midcontinent Rift system}, author = {Hayes, J M and Pratt, L M and Knoll, A H}, abstractNote = {The older assemblages stand in contrast with the ca. 1000 Ma old Hunting Formation, Arctic Canada, which contains what may be the oldest evidence for modem algae - red algal fossils that compare closely with members of ... The Proterozoic Midcontinent Rift System of North Americ

The thickness of the sedimentary cover increases from 0 in the north to over 40,000 ft in the south. In the northern and central parts of the region, remains of a Precambrian rift zone provide the basis for a hypothetical play (Precambrian Midcontinent Rift System).Sep 30, 2019 · The Midcontinent Rift System (MRS) is a Late Mesoproterozoic (∼1.1 Ga) sequence of volcanic and sedimentary rocks exposed in the Lake Superior Region of North America. The MRS continues to be the focus of much research due to its economic mineral deposits as well as its archive of Precambrian life and tectonic processes. Explore the United States' Mountain region and its diverse landscape, rivers, and settlement Learn how the world is divided into continents How the billion-year-old Midcontinent Rift helped form Lake Superior.The structure and geometry of the 1.1-b.y.-old Midcontinent Rift system under Lake Superior is interpreted from 20 seismic reflection profiles recorded during the early and mid-1980s. The seismic ...

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.Midcontinent rift system basalts: Implications for multiple mantle sources during rift devel-opment: Canadian Journal of Earth Sciences, v. 34, p. 504-520, doi: 10 .1139 /e17 -041 .…

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The The Kansas portion of the 1.1-Ga Midcontinent Rift System formed within older cratonic terranes. High-grade metamorphic and granitoid rocks of the Central Plains orogen ranging in age from 1.63 to 1.80 Ga (Sims and Peterman, 1986) constitute the basement in roughly the northern half of the study area. Rhyolitic to dacitic volcanic rocks and ...The last developmental phase of the Midcontinent rift system, from 1.060 to 1.040 Ga, was characterized by a regional compressional event likely caused by continental collision along the Grenville ...Geophysical investigations and crustal structure of the North American Midcontinent Rift system

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 …The Midcontinent Rift system of North America extends for more than 2000 km northeasterly from Kansas through the Lake Superior region and then southeasterly through lower Michigan. The rift has been postulated to be the result of a mantle plume, based on the enormous volume of dominantly

Magmatic Ni-Cu-PGE mineralization in the ~ 1.1 Ga Midcontinent 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) or Keweenawan Rift is a 2,000 km (1,200 mi) long geological rift in the center of the North American continent and south-central part of the North American plate. It formed when the continent's core, the North American craton, began to split apart during the Mesoproterozoic era of the Precambrian, about 1.1 billion years ago. The rift failed, leaving behind ... Over the course of about 10 million years, Recent studies have proposed the existence of several maj The Mid-Continent Rift formed the Lake Superior Basin as continent tried to split into pieces. Younger sedimentary rocks filled in on top of the volcanic rocks as the mountains eroded and rivers flowed into the rift basin. ... The Western arm of the rift system contains the "African Great Lakes" which include some of the deepest lakes in the ...Keweenawan Supergroup. The Keweenawan Supergroup is a supergroup of volcanic and sedimentary rocks that fill the Midcontinent Rift System in the U.S. states of Michigan, Wisconsin, and Minnesota. [1] [2] It is about 30 kilometers (19 mi) thick and it formed about 1.1 billion years ago. [3] The Midcontinent rift system extends from 800 miles from near A Between 1091 and 1098 Ma, most of a 15- to 20-km thickness of dominantly tholeiitic basalt erupted in the Midcontinent Rift System of the Lake Superior region, North American. The Portage Lake Volcanics in Michigan, which are the youngest MRS flood basalts, fall into distinctly high- and low-TiO{sub 2} types having different liquid lines of ...A 70‐km‐long seismic reflection profile in western Michigan provides new insight into the nature, distribution, and structure of the Keweenawan Supergroup volcanic and overlying sedimentary rocks and the controversial Keweenaw fault along the southern boundary of the Midcontinent Rift System in the Lake Superior basin. Interpretation of the 5‐s reflection data constrained by surface ... Precise resolution of the timing of igneous activity is crucial to Feb 27, 2013 · 1 Introduction [2] The Mid-Continent Rift SysThe resistivity signature of the 1.1 Ga Mid-continent The 1100 Ma Midcontinent rift system of North America is one of the world's great igneous provinces, containing over one million km of mafic volcanic and plutonic rocks. Volcanic rocks range from picrite to rhyolite, although tholeiitic basalt predominates. Plutonic rocks range from peridotite to granite, with plagioclase-rich gabbros and ... Abstract. The Midcontinent Rift System (MRS) formed a The Texaco 1 Poersch well in Kansas (11,300 ft TD) was the first significant exploration test of the Mid-Continent Rift System (MRS). An upper succession of rift-related rocks (2846-7429 ft) contains approximately 90% mafic igneous rocks with minor pegmatites and 10% oxidized siltstone and arkose. Arkose and subarkose with minor siltstone and ...Paces J B, Miller J D. Precise U-Pb ages of Duluth Complex and related mafic intrusions, northeastern Minnesota: Geochronological insights into physical, petrogenetic, paleomagnetic, and tectonomagmatic processes associated with the 1.1 Ga midcontinent rift system. J Geophys Res, 1993, 98: 13997-14013 Jun 26, 2023 · Both sites are located alPrecise resolution of the timing of igneous activity is cr ... Mid-Continent Rift System (MCRS). The rift failed, leaving a 2000 km long belt of volcanic and sedimentary rocks left from the early rifting stage. We have ...