Journal ArticleDOI
Alteration zonation and short wavelength infrared (SWIR) characteristics of the Honghai VMS Cu-Zn deposit, Eastern Tianshan, NW China
TLDR
The Honghai VMS Cu-Zn deposit is located in the Dananhu-Tousuquan arc, Eastern Tianshan, northwestern China as mentioned in this paper, and detailed drill core logging, petrographic study and electron microprobe analyses had delineated six alteration/mineralization zones.About:
This article is published in Ore Geology Reviews.The article was published on 2017-03-24. It has received 35 citations till now. The article focuses on the topics: Phyllic alteration & Propylitic alteration.read more
Citations
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Metallogenesis of the Xinjiang Orogens, NW China – New discoveries and ore genesis
TL;DR: In this paper, the authors present the first collective work of Xinjiang mineral resources in international journals, which represents the latest research findings on key Au, Cu, Fe-(Cu), Pb-Zn and other metal deposits in Xinjiang.
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Significance of adakites in petrogenesis of early Silurian magmatism at the Yudai copper deposit in the Kalatag district, NW China
Lei Chen,Lei Chen,Jing Bin Wang,Jing Bin Wang,Leon Bagas,Xiang Bin Wu,Xiang Bin Wu,Hai Yang Zou,Hai Yang Zou,Hui Qiong Zhang,Yan Sun,Xiao Qiang Lv,Xiao Hua Deng +12 more
TL;DR: Yudai is a newly discovered copper deposit associated with a porphyritic quartz diorite, in the Kalatag district of the eastern Tianshan, China.
Journal ArticleDOI
A review of Cu-dominant mineral systems in the Kalatag district, East Tianshan, China
TL;DR: In this article, Li et al. proposed that the north-dipping subduction of the Paleo-Tianshan Ocean during Late Ordovician-Silurian, which may led to the development of Yudai porphyry copper, Hongshi epithermal copper and Honghai VMS copper-zinc deposits in the Kalatag arc.
Journal ArticleDOI
Hydrothermal alteration and short wavelength infrared (SWIR) characteristics of the Tongshankou porphyry-skarn Cu-Mo deposit, Yangtze craton, Eastern China
Jinsheng Han,Jinsheng Han,Gaobin Chu,Huayong Chen,Huayong Chen,Pete Hollings,Siquan Sun,Mi Chen +7 more
TL;DR: In this paper, short wave-length infrared (SWIR) analysis identified 15 hydrothermal minerals in the Tongshankou deposit, including illite, dickite, halloysite, phengite, talc, muscovite, saponite, gypsum, chlorite, prehnite, montmorillonite, serpentine, phlogopite, actinolite, kaolinite.
Journal ArticleDOI
Alteration mapping with short wavelength infrared (SWIR) spectroscopy on Xiaokelehe porphyry Cu-Mo deposit in the Great Xing’an Range, NE China: Metallogenic and exploration implications
Yuzhou Feng,Bing Xiao,Rucao Li,Changzhou Deng,Jinsheng Han,Chao Wu,Guanghui Li,Huilin Shi,Chun-Kit Lai +8 more
TL;DR: In this article, the authors present new data on the alteration mineralogy, vein paragenesis, sulfide assemblages and SWIR (short wavelength infrared) spectroscopy at Xiaokelehe, and discuss how SWIR spectral data can help to understand hydrothermal fluid evolution and assist PCD exploration.
References
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Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia
TL;DR: A new tectonic model, postulating the growth of giant subduction-accretion complexes along a single magmatic arc now found contorted between Siberia and Baltica, shows that Asia grew by 5.3 million square kilometres during the Palaeozoic era as mentioned in this paper.
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Porphyry Copper Systems
TL;DR: Porphyry Cu systems are the most widely distributed mineralization types at convergent plate boundaries, including porphyry deposits centered on intrusions; skarn, carbonate-replacement, and sediment-hosted Au deposits in increasingly peripheral locations; and superjacent high and intermediate-sulfidation epithermal deposits as mentioned in this paper.
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Massive granitoid generation in Central Asia: Nd isotope evidence and implication for continental growth in the Phanerozoic
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Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage
TL;DR: In this paper, an up-to-date along-strike synthesis of the Tianshan orogenic collage and a new tectonic model to explain its accretionary evolution is provided.
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A new review of the chlorites
TL;DR: The chlorites form an extensive isostructural series with a high degree of isomorphous substitution, within which it has always been difficult to define or delimit species; until recently, owing to the lack of adequate X-ray studies, several structurally distinct species were included with the group, further complicating the problem as mentioned in this paper.