Zobrazeno 1 - 10
of 252
pro vyhledávání: '"Jian-Feng Gao"'
Autor:
Ai-Cheng Zhang, Noriyuki Kawasaki, Huiming Bao, Jia Liu, Liping Qin, Minami Kuroda, Jian-Feng Gao, Li-Hui Chen, Ye He, Naoya Sakamoto, Hisayoshi Yurimoto
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-7 (2020)
The authors here analyse the petrology of the meteorite NWA 8321 (parent body Vesta). They find sulfidation processes of olivine suggesting metasomatism in the Vestan interior and a partial melting origin for the host noritic diogenite.
Externí odkaz:
https://doaj.org/article/ec8af426024744a6ad7b501c444517af
Publikováno v:
PLoS ONE, Vol 12, Iss 2, p e0171536 (2017)
The Cathaysia Block is located in southeastern part of South China, which situates in the west Pacific subduction zone. It is thought to have undergone a compression-extension transition of the continental crust during Mesozoic-Cenozoic during the su
Externí odkaz:
https://doaj.org/article/b36b9d1a219a44f28eb90982662d0c70
Publikováno v:
Acta Geochimica. 42:221-240
Autor:
Bingxia Peng, Guochun Zhao, Limin Wu, Bingbing Liu, Touping Peng, Xiaohan Dong, Shili Peng, Weiming Fan, Jian-Feng Gao
Publikováno v:
GSA Bulletin. 135:351-366
South China, India, and their derivative blocks preserve many similar magmatic and sedimentary records related to the tectonic transition from Rodinia to Gondwana. They provide crucial insights into not only the paleogeographic correlation between th
Autor:
Kang Min, Jian-Feng Gao
Publikováno v:
Acta Geochimica. 41:165-184
Autor:
Long-Gang Gao, Rui-Zhong Hu, You-Wei Chen, Xian-Wu Bi, Jian-Feng Gao, Shao-Hua Dong, Jin-Cheng Luo
Publikováno v:
Ore Geology Reviews. 157:105450
Publikováno v:
GSA Bulletin. 134:526-544
The magmatic processes beneath the active continental margins are very complicated and affect structures and compositions of the arc roots. Neoproterozoic igneous rocks are widely distributed around the margins of the Tarim Block in NW China. The Xin
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Publikováno v:
Geological Magazine. 158:1269-1288
Situated between the South China Block and the Simao Block, the Ailaoshan Belt is a significant component of the Jinshajiang–Ailaoshan tectonic-magmatic-metallogenic belt of southwestern China. The formation of the Ailaoshan Belt is closely related
Publikováno v:
Journal of Analytical Atomic Spectrometry. 36:64-69
This study describes an improved alkaline fusion technique for the Re–Os dating of molybdenite. The molybdenite sample was digested in a zirconium crucible with NaOH and carbonized flour at 700 °C. The flour can reduce Os from a high oxidation sta