Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Jingbin Wang"'
Autor:
Lingli Long, Jingbin Wang, Xiao-Hua Deng, Zhi-yuan Sun, Yuwang Wang, Qi-Tao Hu, Zhaohua Luo, Meng-Long Wang
Publikováno v:
Geoscience Frontiers, Vol 11, Iss 2, Pp 697-713 (2020)
The volcanic rocks hosting the iron deposits in the Aqishan–Yamansu metallogenic belt are sodium-rich. The geochronology, petrography, and geochemistry of minerals and sodium-rich rocks as well as the relationship between these rocks and the iron d
Autor:
Yan Sun, Xiaoqiang Lv, Qigui Mao, Jingbin Wang, Yuwang Wang, Lingli Long, Mingjie Yu, Yuechen Li
Publikováno v:
Ore Geology Reviews. 109:598-614
The early Permian Cu–Ni sulfide-bearing mafic-ultramafic intrusions from North Xinjiang in NW China help to provide constraints on the late Paleozoic crustal growth in the Central Asian Orogenic Belt (CAOB) and improve the understanding of the gene
Publikováno v:
Ore Geology Reviews. 107:72-86
The Kalatage area, located in the middle of the Dananhu arc in the Eastern Tianshan, NW China, contains abundant and different types of mineralization , e.g. volcanogenic massive sulfide (VMS) Cu-Zn deposits, porphyry Cu (-Au) deposits and volcanic h
Publikováno v:
Ore Geology Reviews. 104:620-627
The Sareke Cu deposit in the western Tarim region (Xinjiang, NW China) is hosted in continental sedimentary rocks of the Upper Jurassic Kuzigongsu Formation and Lower Cretaceous Kezilesu Group. Stratabound orebodies occur mainly in conglomerate and m
Autor:
Yan Sun, Yuechen Li, Mingjie Yu, Xiaoqiang Lü, Jingbin Wang, Lingli Long, Lei Chen, Yuwang Wang
Publikováno v:
Ore Geology Reviews. 100:220-236
Although the Eastern Tianshan terrane in Xinjiang, NW China, occupies a critical position in the Central Asian Orogenic Belt (CAOB), the early Paleozoic tectonic evolution and mineralization history of this terrane remain ambiguous. The Yudai deposit
Autor:
Lian-Hui Dong, Xiao-Hua Deng, Zhen Zheng, Su-Wei Yue, Chao Li, Jingbin Wang, Hao-Shu Tang, Hong-Jin Chen, M. Santosh, Xun Qu, Yan-Jing Chen
Publikováno v:
Ore Geology Reviews. 80:332-351
The Xiaobaishitou W (–Mo) deposit is located in the eastern segment of the Central Tianshan, northwestern China. The deposit represents a skarn system distributed in the contact zones of biotite granite and crystalline limestone of the Mesoproteroz
Publikováno v:
Ore Geology Reviews. 122:103473
The Xiaoriquanzi volcanogenic massive sulfide (VMS) Cu-Zn deposit occurs at the western part of the Paleozoic Dananhu-Haerlik arc in the eastern Tianshan, Xinjiang, China. Due to a lack of precise mineralization ages, the metallogenesis of the deposi
Publikováno v:
Journal of Asian Earth Sciences. Elsevier Limited
Although there are important implications for mineral exploration, the genetic links between porphyry Mo and peripheral Mo–Cu vein deposits remain unclear. To constrain their possible relationships, this paper studied hydrothermal veins, Ar–Ar ge
Publikováno v:
Gondwana Research. 22:534-553
We report newly-defined Nb-enriched basalts, adakites and dacites from the Beishan, NW China of the southern Altaids based on field, geochemical, isotopic and geochronology studies. Two phases of adakites (adakite-I and adakite-II) have been defined,
Autor:
Huawu Dai, Heping Zhu, Jingbin Wang, Lian-Hui Dong, Yuanchao Shen, Xian-Hua Li, Weina Guan, Ping Shen, Hongdi Pan
Publikováno v:
Journal of Asian Earth Sciences. 49:99-115
The Baogutu copper deposit, a newly-discovered middle-sized porphyry copper deposit, is located in the West Junggar region of Xinjiang, NW China. Baogutu is associated with a Late Carboniferous intrusive complex that was emplaced into Lower Carbonife