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Yanbo Cheng
James Cook University
37Publications
13H-index
385Citations
Publications 37
Newest
Published on Jan 1, 2019in American Mineralogist 2.65
Yanbo Cheng13
Estimated H-index: 13
(JCU: James Cook University),
Carl Spandler27
Estimated H-index: 27
(JCU: James Cook University)
+ 4 AuthorsKevin Blake1
Estimated H-index: 1
(WWU: Western Washington University)
1 Citations Source Cite
Published on Mar 1, 2018in Earth and Planetary Science Letters 4.58
Yanbo Cheng13
Estimated H-index: 13
(JCU: James Cook University),
Carl Spandler27
Estimated H-index: 27
(JCU: James Cook University)
+ 1 AuthorsGavin W. Clarke3
Estimated H-index: 3
(JCU: James Cook University)
Abstract Understanding the connection between the highly evolved intrusive and extrusive systems is essential to explore the evolution of high silicic magma systems, which plays an important role in discussions of planetary differentiation, the growth of continents, crustal evolution, and the formation of highly evolved magma associated Sn–W–Mo mineral systems. To discern differences between “fertile” and “non-fertile” igneous rocks associated with Sn–W–Mo mineralization and reveal the genetic l...
4 Citations Source Cite
Published on Aug 1, 2017in Lithos 3.86
Jingwen Mao33
Estimated H-index: 33
,
Bikang Xiong2
Estimated H-index: 2
+ 5 AuthorsPan Dai1
Estimated H-index: 1
Abstract The Yangchuling W–Mo deposit, located in the Jiangnan porphyry–skarn (JNB) tungsten ore belt, is the first recognized typical porphyry W–Mo deposit in China in the 1980's. Stockworks and disseminated W–Mo mineralization occur in the roof pendant of a 0.3 km 2 monzogranitic porphyry stock that intruded into a granodiorite stock, hosted by Neoproterozoic phyllite and slate. LA-ICPMS zircon U–Pb analyses suggest that of the monzogranitic porphyry and granodiorite were formed at 143.8 ± 0.5...
22 Citations Source Cite
Published on Mar 1, 2017in Ore Geology Reviews 3.99
Peng Liu3
Estimated H-index: 3
(China University of Geosciences),
Jingwen Mao33
Estimated H-index: 33
+ 3 AuthorsDi Hao1
Estimated H-index: 1
(China University of Geosciences)
Abstract The Feie'shan W-Sn deposit is in eastern Guangdong Province, which is a newly explored deposit in the southeastern coastal metallogenic belt. In order to constrain the age of mineralization in the Feie'shan W-Sn deposit, we collected molybdenites and hydrothermal biotite of the Feie'shan W-Sn deposit for dating. The tungsten mineralization is spatially associated with the biotite monzonitic granite porphyry. LA-MC-ICP-MS zircon U-Pb dating of the biotite monzonitic granite porphyry yiel...
15 Citations Source Cite
Published on Jan 1, 2017
Zhaoshan Chang15
Estimated H-index: 15
,
Gavin W. Clarke3
Estimated H-index: 3
+ 2 AuthorsK. Liu
Deposits with economic tin (Sn) or tungsten (W) – molybdenum (Mo) are widespread in north-east Queensland, ranging between -14.40 and -19.50°and 143.50-146.20°. This area used to be one of the major sources on Sn and W in Australia, with mineralisation discovered and exploited from the 1880s. According to the Geological Survey of Queensland (GSQ) database (von Gnielinski, 2015) this region has 792 Sn deposits and 132 W deposits. The large number indicates that geological conditions are generally...
Published on Dec 1, 2016in Solid Earth Sciences
Yanbo Cheng13
Estimated H-index: 13
(JCU: James Cook University),
Jingwen Mao33
Estimated H-index: 33
(China University of Geosciences),
Peng Liu3
Estimated H-index: 3
(China University of Geosciences)
The Sn–W mineralization in SE Yunnan Province, China and NE Vietnam shares many similarities. Through comparing the geological and geochronological data, we suggest the Sn–W deposits and the associate igneous rocks in the region represent one regional magmatic-mineralization event. To explore the geodynamic setting of these mineralization and magmatic activities, a geochronological dataset in the regions has been presented, containing data of this study and previously published. The dataset show...
16 Citations Source Cite
Published on May 1, 2015in Journal of Asian Earth Sciences 2.87
Jingwen Mao33
Estimated H-index: 33
,
Franco Pirajno48
Estimated H-index: 48
+ 2 AuthorsYanbo Cheng13
Estimated H-index: 13
[Extract] Professor Yuchuan Chen, born in December 7, 1934, in Pinghu city of Zhejiang province, China, is an economic geologist well known not only in China but all over the world. He graduated from the Donetsk National University in 1959. From that time he has devoted himself to the fields of economic geology, geochemistry, regional metallogeny, mineral prospecting and exploration for 60 years.
4 Citations Source Cite
Published on May 1, 2015in Journal of Asian Earth Sciences 2.87
Hou-Min Li7
Estimated H-index: 7
,
Li-Xing Li7
Estimated H-index: 7
+ 1 AuthorsYanbo Cheng13
Estimated H-index: 13
China has the largest global demand for iron ore resources, with more than 50% of its demand presently being met from foreign sources. Iron resources are abundant in China (ca. 80 billion tons of proven iron ores), but high-grade ores are scarce. Most iron deposits in China are low in grade, with an average grade of 30.62% TFe. The iron deposits in China are divided into six types: sedimentary–metamorphic, magmatic Fe–Ti–(V), volcanic rock-hosted, contact metasomatic–hydrothermal (mostly skarn),...
14 Citations Source Cite
Published on May 1, 2015in Journal of Asian Earth Sciences 2.87
Yue Wang4
Estimated H-index: 4
,
Xiangkun Zhu7
Estimated H-index: 7
,
Yanbo Cheng13
Estimated H-index: 13
Abstract Fe isotope compositions of mineral separates and bulk samples from Dongguashan and Fenghuangshan skarn type Cu–Fe deposits in Tongling District, Middle–Lower Yangtze Valley Cu–Fe–Au–Mo polymetallic belt have been investigated. Differences in δ 57 Fe values exist in co-precipitated bornite–chalcopyrite and pyrite–chalcopyrite mineral pairs. The bornite is enriched in light iron isotopes relative to coexisting chalcopyrite, whereas pyrite samples show a tendency of heavy isotopes enrichme...
9 Citations Source Cite
Published on Apr 1, 2015in Gondwana Research 5.66
Yanbo Cheng13
Estimated H-index: 13
(China University of Geosciences),
Jingwen Mao33
Estimated H-index: 33
(China University of Geosciences)
+ 1 AuthorsYue Wang4
Estimated H-index: 4
Abstract Fe isotope compositions of bulk samples from Gaosong ore deposit in Gejiu district, SW China were investigated and an overall variation in δ 56 Fe values from − 0.33‰ to + 0.20‰ has been observed. In this study, the δ 56 Fe values of primary sulfide ores are lower than the oxidized ores, while the iron isotope compositions of gossan samples, which represent highest oxidation degree, are heavier than the oxidized ore samples. These data indicate that iron isotopes experienced fractionati...
15 Citations Source Cite
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