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Bing Xiao
Chinese Academy of Sciences
18Publications
7H-index
191Citations
Publications 18
Newest
#1Yunfeng Wang (CAS: Chinese Academy of Sciences)H-Index: 4
#2Huayong Chen (CAS: Chinese Academy of Sciences)H-Index: 21
Last.Fred Jourdan (Curtin University)H-Index: 36
view all 7 authors...
The Tuwu porphyry Cu deposit, located in Eastern Tianshan, NW China, is hosted by a plagiogranite porphyry and Carboniferous Qi’eshan Group volcanic rocks. Based on crosscutting relationships and mineral assemblages, hydrothermal alteration and mineralization processes at Tuwu can be divided into four stages: early propylitic alteration (stage I), porphyry mineralization (stage II), overprinting mineralization (stage III), and post-mineralization (stage IV). The porphyry mineralization stage (st...
2 CitationsSource
#1Yuzhou Feng (CAS: Chinese Academy of Sciences)H-Index: 2
#2Bing Xiao (CAS: Chinese Academy of Sciences)H-Index: 7
Last.Chun-Kit Lai (UBD: Universiti Brunei Darussalam)H-Index: 11
view all 9 authors...
Abstract The newly discovered Xiaokelehe porphyry Cu-Mo deposit (PCD) is situated in northern part of the Great Xing’an metallogenic belt, northeastern China. The syn-mineralization granodiorite porphyry was intruded by multiple phases of post-ore barren monzonite, diorite porphyry and granite porphyry, leading to complex and overprinting hydrothermal alteration patterns. This paper present new data on the alteration mineralogy, vein paragenesis, sulfide assemblages and SWIR (short wavelength in...
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#1Changzhou Deng (JLU: Jilin University)H-Index: 3
#2SUNDeyou (JLU: Jilin University)H-Index: 19
Last.Dong-Guang Yang (JLU: Jilin University)H-Index: 3
view all 10 authors...
Abstract The genesis of igneous rocks associated with the newly discovered Xiaokele porphyry Cu-Mo deposit, located in the eastern Erguna Block, NE China, can give insights into the regional geodynamic evolution during the Late Mesozoic. Several ore-bodies have been indentified in a granodiorite porphyry stock, which intruded the rhyolite and was subsequently intruded by diorite porphyry and granite porphyry. The U–Pb ages of zircons from rhyolite, mineralized granodiorite porphyry, diorite porp...
3 CitationsSource
#1Jianping Li (CAS: Chinese Academy of Sciences)H-Index: 1
#2Huayong Chen (CAS: Chinese Academy of Sciences)H-Index: 21
Last.Yunfeng Wang (CAS: Chinese Academy of Sciences)H-Index: 4
view all 5 authors...
Porphyry copper systems, which provide most of the world’s copper resource, are commonly associated with characteristic concentric zonation of alteration and mineralization. In-depth knowledge of the distribution and transport mechanism of elements in the alteration zones is essential for understanding the ore-forming processes. We employed flow-reaction apparatus to simulate the fluid-rock interactions during porphyry ore formation so as to investigate the mechanisms that govern the transport o...
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#1Changzhou Deng (JLU: Jilin University)H-Index: 3
#2SUNDeyou (JLU: Jilin University)H-Index: 19
Last.Sheng Lu (JLU: Jilin University)H-Index: 3
view all 10 authors...
Abstract Multistage igneous rocks identified in the newly discovered Fukeshan porphyry Cu Mo deposit, NE China give new insights into the late-stage southwards subduction of the Mongol-Okhotsk oceanic slab (MOOS) and Cu Mo mineralization during the late Mesozoic. The U Pb ages of zircons from medium-grained monzogranite, coarse-grained monzogranite, ore-related quartz diorite porphyry, quartz monzonite, ganodiorite porphyry, diorite porphyry and andesitic porphyry associated with the Fukeshan de...
5 CitationsSource
#1Jinsheng Han (CAS: Chinese Academy of Sciences)H-Index: 8
#2Huayong Chen (CAS: Chinese Academy of Sciences)H-Index: 21
Last.Zhixiong TanH-Index: 3
view all 9 authors...
Abstract Two populations of zircons are present in the F-rich highly evolved 300 Ma Shuangji granites, Xinjiang, eastern Tianshan, China. Zircon I comprise a very small proportion of the population. They show characteristics of primary igneous zircons and yield an age of ca. 300 Ma. Zircon II are the dominant type and are weakly luminescent under cathodoluminescence (CL) but show a range of complex textures in back-scattered electron (BSE) images. Zircon II are characterized by Th-U-rich mineral...
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#1Bing Xiao (CAS: Chinese Academy of Sciences)H-Index: 7
#2Huayong Chen (CAS: Chinese Academy of Sciences)H-Index: 21
Last.Fangyue Wang (Hefei University of Technology)H-Index: 2
view all 6 authors...
Abstract Chlorite is one of the most widely developed minerals in propylitic alteration around porphyry deposits and can be used to investigate element transport and enrichment processes during hydrothermal alteration. The Paleozoic Tuwu porphyry Cu deposit (metal reserve: 0.7 Mt Cu @ 0.67%), located in the southern margin of the Central Asian Orogenic Belt, is one of the most economical and largest porphyry Cu deposits in NW China. The Tuwu porphyry Cu deposit comprises an early porphyry Cu min...
1 CitationsSource
#1Huayong Chen (CAS: Chinese Academy of Sciences)H-Index: 21
#2Wan Bo (CAS: Chinese Academy of Sciences)H-Index: 23
Last.Bing Xiao (CAS: Chinese Academy of Sciences)H-Index: 7
view all 5 authors...
Abstract The Xinjiang Uygur Autonomous Region in NW China occupies around 1/6 of the total China land size, and contains components of both the Central Asian Orogenic Belt (CAOB) and Paleo-Tethyan Orogenic Belt (PTOB). The Paleozoic CAOB is situated in the northern and central parts of Xinjiang, whilst the Paleozoic-Mesozoic PTOB is mainly located in the southern part of Xinjiang. These orogenic belts were formed by the multiphase Paleozoic-Mesozoic terrane accretions and collisions enacted by t...
5 CitationsSource
#1Wanjian Lu (CAS: Chinese Academy of Sciences)H-Index: 7
#2Huayong Chen (CAS: Chinese Academy of Sciences)H-Index: 21
Last.Hongjun Jiang (CAS: Chinese Academy of Sciences)H-Index: 3
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Abstract The Central Tianshan Terrane (CTT) in the Eastern Tianshan (Xinjiang, NW China) is an important Pb–Zn metallogenic belt and played a pivotal role in crustal evolution and collisional tectonics of the southern Central Asian Orogenic Belt. The Shaquanzi gabbro and Hongyuan granodiorite are located in the northern margin of the CTT and associated with Pb–Zn mineralization. Zircon U–Pb dating yielded weighted mean ages of 307.2 ± 1.5 Ma and 301.2 ± 1.5 Ma for the Shaquanzi gabbro and the Ho...
3 CitationsSource
#1Yunfeng Wang (CAS: Chinese Academy of Sciences)H-Index: 4
#2Huayong Chen (CAS: Chinese Academy of Sciences)H-Index: 21
Last.Fred Jourdan (Curtin University)H-Index: 36
view all 7 authors...
Abstract The Yandong porphyry copper deposit is located in the southern part of the Dananhu-Tousuquan Island Arc belt in Eastern Tianshan (Xinjiang, NW China). The Dananhu-Tousuquan belt contains a number of large and medium Cu deposits, among which the Yandong deposit (∼2.0 Mt Cu @ 0.67%) is the largest. The Yandong Cu deposit is hosted by plagiogranite porphyry and the Carboniferous Qi’eshan Group mafic to intermediate calc-alkaline volcanic and pyroclastic rocks. According to the crosscutting...
6 CitationsSource
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