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Richard W. Carlson
Carnegie Institution for Science
GeologyCratonBasaltGeochemistryMantle (geology)
287Publications
64H-index
12.6kCitations
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Publications 282
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#1Richard W. Carlson (CIS: Carnegie Institution for Science)H-Index: 64
Compositional signatures of subducted crust in the deep-mantle sources of ocean island volcanoes in the Atlantic Ocean but not the Pacific reveal that plate motions on Earth’s surface influence the characteristics of Earth’s deepest interior.
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#1J. R. Reimink (PSU: Pennsylvania State University)H-Index: 7
#2Andrea Mundl‐Petermeier (UMD: University of Maryland, College Park)H-Index: 1
Last. D. Graham Pearson (U of A: University of Alberta)H-Index: 23
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#1N. E. Moore (OSU: Oregon State University)H-Index: 1
#2Anita L. Grunder (OSU: Oregon State University)H-Index: 23
Last. Ilya N. Bindeman (UO: University of Oregon)H-Index: 46
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#1Ji Shen (USTC: University of Science and Technology of China)H-Index: 6
#2Jiuxing Xia (ZJU: Zhejiang University)H-Index: 1
Last. T. D. Mock (CIS: Carnegie Institution for Science)H-Index: 10
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Abstract The stable isotope compositions of chromium (Cr) are fractionated during magmatic differentiation of lunar mare basalts, which might be attributed to redox-related mineral crystallization. It has yet to be demonstrated whether magmatic differentiation fractionates Cr isotope composition of terrestrial samples. Here, we present high-precision stable Cr isotope measurements, reported as δ53Cr relative to NIST SRM 979, of well-characterized Hawaiian tholeiitic basalts from Koolau, Mauna Ke...
2 CitationsSource
#1Arto V. LuttinenH-Index: 2
#2Jussi S. HeinonenH-Index: 11
Last. Mary F. Horan (CIS: Carnegie Institution for Science)H-Index: 31
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#1J. R. ReiminkH-Index: 7
#2D.G. PearsonH-Index: 3
Last. J.W.F. KetchumH-Index: 1
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#1Richard W. Carlson (CIS: Carnegie Institution for Science)H-Index: 64
#2Marion GarçonH-Index: 12
Last. Hanika Rizo (Carleton University)H-Index: 8
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Abstract Recycling of crust into the mantle has left only small remnants at Earth’s surface of crust produced within a billion years of Earth formation. Few, if any, of these ancient crustal rocks represent the first crust that existed on Earth. Understanding the nature of the source materials of these ancient rocks and the mechanism of their formation has been the target of decades of geological and geochemical study. This traditional approach has been expanded recently through the ability to s...
2 CitationsSource
#1Nicole E. MooreH-Index: 1
Last. Wendy A. BohrsonH-Index: 22
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#1Richard W. CarlsonH-Index: 64
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#1Jun Hu (CAS: Chinese Academy of Sciences)H-Index: 34
#2Neng Jiang (CAS: Chinese Academy of Sciences)H-Index: 21
Last. Huimin Yu (USTC: University of Science and Technology of China)H-Index: 11
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Abstract Substantial quantities of sediments are known to enter the deep lithosphere at subduction zones, but the extent to which sediments melt and the process involved in sediment contribution to the deep lithosphere are inadequately understood. Vigorous debate continues about whether the subducted sediment component is terrigenous or pelagic and transported as a hydrous melt, an aqueous fluid, or bulk sediment. In this contribution, we conduct an integrated study on a variety of deep-seated x...
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