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Li-Hui Chen
Nanjing University
GeologyBasaltGeochemistryMagmaMantle (geology)
36Publications
14H-index
768Citations
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Publications 34
Newest
#1Ai-Cheng Zhang (Center for Excellence in Education)H-Index: 8
#2Noriyuki Kawasaki (Hokkaido University)H-Index: 6
Last. Naoya Sakamoto (Hokkaido University)H-Index: 43
view all 11 authors...
Diogenites are a group of meteorites that are derived from the interior of the largest protoplanet Vesta. They provide a unique opportunity to understanding together the internal structure and dynamic evolution of this protoplanet. Northwest Africa (NWA) 8321 was suggested to be an unbrecciated noritic diogenite meteorite, which is confirmed by our oxygen and chromium isotopic data. Here, we find that olivine in this sample has been partly replaced by orthopyroxene, troilite, and minor metal. Th...
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#1Saskia Erdmann (University of Orléans)H-Index: 11
#2Li-Hui Chen (NU: Nanjing University)H-Index: 14
Last. Xi Wang (NU: Nanjing University)H-Index: 6
view all 5 authors...
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#1Ye He (NU: Nanjing University)
#2Li-Hui Chen (Center for Excellence in Education)H-Index: 14
Last. Lie-Wen Xie (CAS: Chinese Academy of Sciences)H-Index: 30
view all 9 authors...
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#1Xun Yu (Tongji University)H-Index: 7
#2Gang Zeng (NU: Nanjing University)H-Index: 9
Last. Zhi-Qiang Yu (NU: Nanjing University)
view all 5 authors...
ABSTRACTRecently, besides magma–rock and rock–rock reaction, magma–magma interaction at mantle depth has been proposed as an alternative mechanism to produce diverse compositions of mantle. Clinopy...
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#1Xun Yu (Tongji University)H-Index: 7
#2Gang Zeng (NU: Nanjing University)H-Index: 9
Last. Tao Yang (NU: Nanjing University)H-Index: 13
view all 7 authors...
Abstract Cenozoic intraplate basalts are widely distributed along the southeastern margin of Eurasia. Both carbonated and eclogitic/pyroxenitic components, which are considered related to oceanic crust recycling, have been identified in the mantle source of these basalts. However, the origin of the recycled oceanic crust and the genetic relationship between different source lithologies remain unclear. Here, we assess the source lithologies of late Miocene intraplate basalts from Ninghai, Zhejian...
1 CitationsSource
#1Xiao-Jun Wang (NU: Nanjing University)H-Index: 5
#2Li-Hui Chen (NU: Nanjing University)H-Index: 14
Last. Jun-Ichi Kimura (JAMSTEC: Japan Agency for Marine-Earth Science and Technology)H-Index: 36
view all 15 authors...
The extreme Sr, Nd, Hf, and Pb isotopic compositions found in Pitcairn Island basalts have been labeled enriched mantle 1 (EM1), characterizing them as one of the isotopic mantle end members. The EM1 origin has been vigorously debated for over 25 years, with interpretations ranging from delaminated subcontinental lithosphere, to recycled lower continental crust, to recycled oceanic crust carrying ancient pelagic sediments, all of which may potentially generate the requisite radiogenic isotopic c...
7 CitationsSource
#1Ai-Cheng Zhang (NU: Nanjing University)H-Index: 8
#2Yi-Fan Bu (NU: Nanjing University)H-Index: 1
Last. Wang Rucheng (NU: Nanjing University)H-Index: 26
view all 10 authors...
Abstract Troilite-orthopyroxene intergrowths are present as a common material in the brecciated diogenite Northwest Africa (NWA) 7183. In this study, we report on the petrographic, mineralogical, and rare earth element abundances of the troilite-orthopyroxene intergrowths to constrain their origin and assess their implications for the diverse petrogenesis of diogenites. Two groups of troilite-orthopyroxene intergrowths with various grain sizes and mineral chemistry have been observed in NWA 7183...
2 CitationsSource
#1Xun Yu (NU: Nanjing University)H-Index: 7
#2Li-Hui Chen (NU: Nanjing University)H-Index: 14
Last. Gang Zeng (NU: Nanjing University)H-Index: 9
view all 3 authors...
Abstract Isotopic compositions of continental flood basalts are essential to understand their genesis and to constrain the character of their mantle sources. Because of potential crustal contamination, it needs to be evaluated if and to which degree these basalts record original isotopic signals of their mantle sources and/or crustal signatures. This study examines the Sr, Nd, Hf, and Pb isotopic compositions of the late Cenozoic Xinchang–Shengzhou (XS) flood basalts, a small-scale continental f...
4 CitationsSource
#1Xiao-Jun Wang (NU: Nanjing University)H-Index: 5
#2Li-Hui Chen (NU: Nanjing University)H-Index: 14
Last. Yue-Heng Yang (CAS: Chinese Academy of Sciences)H-Index: 43
view all 8 authors...
The isotopic characteristics of the sub-oceanic mantle are well established, but in continental regions these properties are usually obscured, and therefore controversial, because of the potential effects of crustal contamination together with lithospheric mantle metasomatism and melting. The so-called EM1 (Enriched Mantle-1) signature, characterized by low 206Pb/204Pb and 143Nd/144Nd ratios, is particularly problematic in this respect because EM1-type OIB sources are commonly attributed to recy...
29 CitationsSource
#1Gang Zeng (NU: Nanjing University)H-Index: 9
#2Li-Hui Chen (NU: Nanjing University)H-Index: 14
Last. Saskia Erdmann (NU: Nanjing University)H-Index: 11
view all 6 authors...
In addition to magma-rock and rock-rock reaction, magma-magma interaction at mantle depth has recently been proposed as an alternative mechanism to produce the compositional diversity of intraplate basalts. However, up to now no compelling geochemical evidence supports this novel hypothesis. Here we present geochemistry for the Longhai basalts from Fujian Province, southeastern China, which demonstrates the interaction between two types of magma at mantle depth. At Longhai, the basalts form two ...
10 CitationsSource
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