Výsledky vyhledávání - "Zhuangzhi Qian"

Petrogenesis and Ni-Cu exploration potential of Devonian mafic–ultramafic intrusions in the southern part of the Central Asian Orogenic Belt, NW China: constraints from zircon O isotopes and whole-rock Sr-Nd isotopes

Autor: Jiangjiang Zhang, Zhigang Zhang, Zhuangzhi Qian, Bocheng Ma, Jun Duan, Gang Xu, Wenbin Gao

Publikováno v: International Geology Review. 64:1495-1513

Weakly disseminated sulphide mineralization is present in the outcrops of several mafic–ultramafic intrusions in the Beishan region of the Central Asian Orogenic Belt in western China, but the pote...

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3bd68e83d36faaaa33bcd70b2096b505
https://doi.org/10.1080/00206814.2021.1934739

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Petrogenesis of the Permian Luotuoshan sulfide-bearing mafic-ultramafic intrusion, Beishan Orogenic Belt, NW China: evidence from whole-rock Sr–Nd–Pb and zircon Hf isotopic geochemistry

Autor: Gang Xu, Jiangjiang Zhang, Zhuangzhi Qian, Wenbin Gao, Jun Duan, Reid R. Keays, Bocheng Ma

Publikováno v: Journal of Geochemical Exploration. 233:106920

The Permian Luotuoshan mafic-ultramafic intrusion is one of the ∼280 Ma mafic-ultramafic complexes located in the Beishan Orogenic Belt at the southern margin of the Central Asian Orogenic Belt, NW China. The intrusion is predominantly composed of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::2dda8c90974a7847d9294fb5dc947418
https://doi.org/10.1016/j.gexplo.2021.106920

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Paleozoic mafic-intermediate intrusions (320–287 Ma) in the Kalatongke area, southern Altai, NW China: Products of protracted magmatism in a convergent tectonic setting

Autor: Gang Xu, Jun Duan, Chusi Li, Yanqing Feng, Meng Ren, Zhuangzhi Qian

Publikováno v: Journal of Asian Earth Sciences. 159:294-307

Numerous small mafic-intermediate intrusions are present in the Kalatongke area in the southern part of the Paleozoic Altai Orogenic Belt, NW China. Previous studies reveal that most of these intrusions were emplaced at ∼287 Ma, broadly coeval with

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d05ed4da8c620230f15933c1e2dab29d
https://doi.org/10.1016/j.jseaes.2016.12.038

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Geochemical and Petrological Studies on the Early Carboniferous Sidingheishan Mafic-Ultramafic Iintrusion in the Southern Margin of the Central Asian Orogenic Belt, NW China

Autor: Jing Wang, Gang Xu, Zhuangzhi Qian, Tao Sun, Joyashish Thakurta, Jun Duan, Shenghong Yang, Bo Gao

Publikováno v: Acta Geologica Sinica - English Edition. 92:952-971

The Sidingheishan mafic–ultramafic intrusion is located in the eastern part of the Northern Tianshan Mountain, along the southern margin of the Central Asian Orogenic Belt in northern Xinjiang autonomous region of China. The Sidingheishan intrusion

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d1531c511fa5205ebc3217b1bbe92777
https://doi.org/10.1111/1755-6724.13585

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Geochronological and geochemical study of the Baixintan magmatic Ni-Cu sulphide deposit: New implications for the exploration potential in the western part of the East Tianshan nickel belt (NW China)

Autor: Gang Xu, Zhuangzhi Qian, Yanqing Feng, Chao Jiang, Jun Duan, Meng Ren

Publikováno v: Ore Geology Reviews. 95:366-381

Several newly discovered magmatic Ni-Cu sulphide deposits are located in the East Tianshan nickel belt in the southern part of the Central Asian Orogenic Belt in NW China. The Baixintan magmatic sulphide deposit is one of these new discoveries. The h

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::daa1153e8bc4f8070245f05f8f175483
https://doi.org/10.1016/j.oregeorev.2018.02.023

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Compositional variations of several Early Permian magmatic sulfide deposits in the Kalatongke district, southern Altai, western China: With genetic and exploration implications

Autor: Jiangang Jiao, Gang Xu, Chusi Li, Edward M. Ripley, Zhuangzhi Qian, Yanqing Feng, Jun Duan

Publikováno v: Ore Geology Reviews. 90:576-590

A Permian magmatic Ni-Cu sulfide deposit cluster occurs in the Kalatongke district in the Southern Chinese Altai Orogenic Belt, western China. These deposits are associated with the mafic units of the Y1, Y2, Y3, Y9 and G21 mafic-intermediate complex

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::f77c22dfe78e7ce0c89c0ab30ba6909d
https://doi.org/10.1016/j.oregeorev.2017.04.031

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The genesis of the Xujiagou copper deposit, Mian-Lue-Ning area of Shaanxi Province, NW China: Constraints from mineral chemistry and in situ Pb isotope composition

Autor: Kun Ding, Zhuangzhi Qian, Lixiang Chen, Yan Luan, Yongqin Li, Ruiting Wang, Tianyun Zhang

Publikováno v: Geological Journal. 53:44-57

The Mian-Lue-Ning area, bounded by the Hanjiang fault zone in the south and the Mian-Lue suture in the north, is one of the most important polymetallic mineralization concentration regions in the Qinling orogenic belt. The Xujiagou copper deposit is

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9b26f31a6e141b9bf40e76c7aa20f7ca
https://doi.org/10.1002/gj.2994

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Multiple S isotopes, zircon Hf isotopes, whole-rock Sr-Nd isotopes, and spatial variations of PGE tenors in the Jinchuan Ni-Cu-PGE deposit, NW China

Autor: Jiangang Jiao, Chusi Li, Yanqing Feng, Edward M. Ripley, Zhuangzhi Qian, Jun Duan

Publikováno v: Mineralium Deposita. 51:557-574

Previous geochemical data for the Jinchuan Ni-Cu-(platinum-group elements, PGE) deposit, the single largest magmatic sulfide deposit in the world, are derived primarily from the upper parts of the deposit. This paper reports new PGE and S-Hf-Sr-Nd is

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d528e5ddf6d745eab2334218a0d1cf1f
https://doi.org/10.1007/s00126-015-0626-8

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Geochronological and geochemical constraints on the petrogenesis and tectonic significance of Paleozoic dolerite dykes in the southern margin of Alxa Block, North China Craton

Autor: Jiangang Jiao, Zhuangzhi Qian, Jun Duan, Chusi Li

Publikováno v: Journal of Asian Earth Sciences. 111:244-253

Dolerite dykes are common in the southern margin of Alxa Block which is the westernmost part of North China Craton. The ages and petrogenesis of the dolerite dykes, which are important for a better understanding of tectonic–magmatic evolution in th

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::8f2fe7068d50ff0ebd71e608bc2ac272
https://doi.org/10.1016/j.jseaes.2015.07.012

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