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From:Science (Vol. 310, Issue 5754) Peer-ReviewedNot quite 2 billion years ago, a large asteroid stuck itself into what is now eastern central Ontario, forming the Sudbury impact crater. The energy of the impact melted a large amount of the continental crust,...
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From:Science (Vol. 269, Issue 5230) Peer-ReviewedThe Archean crust contains direct geochemical information of the Earth's early planetary differentiation. A major outstanding question in the Earth sciences is whether the volume of continental crust today represents...
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From:Nature (Vol. 484, Issue 7395) Peer-ReviewedAuthor(s): Birger Rasmussen (corresponding author) [1]; Ian R. Fletcher [1]; Andrey Bekker [2]; Janet R. Muhling [3]; Courtney J. Gregory [1]; Alan M. Thorne [4] Iron formations are chemical sedimentary rocks...
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From:Canadian Journal of Earth Sciences (Vol. 53, Issue 12) Peer-ReviewedAbstract: This paper presents results of a laser ablation - inductively coupled plasma - quadrapole mass spectrometer (LA-ICP-QMS) U-Pb dating study of small in situ zircon grains from samples collected in the vicinity...
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From:Contributions to Mineralogy and Petrology (Vol. 168, Issue 3) Peer-ReviewedThe two most commonly invoked processes for generating silicic magmas in intra-oceanic arc environments are extended fractional crystallization of hydrous island arc basalt magma or dehydration melting of lower crustal...
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From:Science (Vol. 297, Issue 5582) Peer-ReviewedEarth's dynamic oblateness ([J.sub.2]) had been undergoing a decrease, according to space geodetic observations over the past 25 years, until around 1998, when it switched quite suddenly to an increasing trend that has...
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From:Science (Vol. 310, Issue 5756) Peer-ReviewedThe long-favored paradigm for the development of continental crust is one of progressive growth beginning at ~4 billion years ago (Ga). To test this hypothesis, we measured initial [sup.176]Hf/[sup.177]Hf values of...
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From:Solid Earth (Vol. 7, Issue 3) Peer-ReviewedTo establish the horizontal crustal movement velocity field of the Chinese mainland, a Hardy multi-quadric fitting model and collocation are usually used. However, the kernel function, nodes, and smoothing factor are...
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From:Solid Earth (Vol. 9, Issue 2) Peer-ReviewedComputing a better crustal thickness model is still a necessary improvement in Antarctica. In this remote continent where almost all the bedrock is covered by the ice sheet, seismic investigations do not reach a...
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From:Scientific Drilling (Vol. 29) Peer-ReviewedFor more than half a century, exploring a complete sequence of the oceanic crust from the seafloor through the Mohorovicic discontinuity (Moho) and into the uppermost mantle has been one of the most challenging missions...
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From:Solid Earth (Vol. 12, Issue 8) Peer-ReviewedThe contemporary stress state in the upper crust is of great interest for geotechnical applications and basic research alike. However, our knowledge of the crustal stress field from the data perspective is limited. For...
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From:Biogeosciences (Vol. 18, Issue 17) Peer-ReviewedExchange of dissolved substances at the sediment-water interface provides an important link between the short-term and long-term geochemical cycles in the ocean. A second, as yet poorly understood sediment-water exchange...
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From:Contributions to Mineralogy and Petrology (Vol. 165, Issue 2) Peer-ReviewedThe petrology and timing of crustal melting has been investigated in the migmatites of the Higher Himalayan Crystalline (HHC) exposed in Sikkim, India. The metapelites underwent pervasive partial melting through hydrous...
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From:Nature (Vol. 580, Issue 7802) Peer-ReviewedA reduction in seismic noise because of changes in human activity is a boon for geoscientists. A reduction in seismic noise because of changes in human activity is a boon for geoscientists. Author(s): Elizabeth...
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From:Science (Vol. 245, Issue 4922) Peer-ReviewedUnderplating and Partial Melting: Implications for Melt Generation and Extraction UNDERPLATING AND INTRUSION OF continental crust by basaltic magma has repeatedly been invoked as a mechanism to provide the needed heat...
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From:Science (Vol. 229) Peer-ReviewedNative Iron in the Continental Lower Crust: Petrological and Geophysical Implications Information on the mineralogy of the deep continental crust is extremely limited (1), and the redox state of the lower crust has...
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From:Science (Vol. 261, Issue 5129) Peer-ReviewedVolume diffusion models predict that crystals with large diffusion dimensions can record a wide range of thermal conditions in the Earth's crust. Direct measurements of the zoning of radiogenic argon-40 in single...
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From:Natural Hazards and Earth System Sciences (Vol. 14, Issue 5) Peer-ReviewedByline: P. Kü,reÃ,§,, H. Konak To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
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From:Canadian Journal of Earth Sciences (Vol. 51, Issue 6) Peer-ReviewedIntegrated mapping, structural analysis, and U-Pb geochronology of the Committee Bay area, Nunavut, establish a record of Neoarchean crustal growth followed by penetrative Paleoproterozoic deformation. Supracrustal...