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David I. Groves
China University of Geosciences
6Publications
1H-index
9Citations
Publications 6
Newest
2018 in Geoscience frontiersIF: 4.05
David I. Groves1
Estimated H-index: 1
(China University of Geosciences),
M. Santosh79
Estimated H-index: 79
(University of Adelaide)
+ 1 AuthorsLiang Zhang1
Estimated H-index: 1
(China University of Geosciences)
Abstract With very few exceptions, orogenic gold deposits formed in subduction-related tectonic settings in accretionary to collisional orogenic belts from Archean to Tertiary times. Their genesis, including metal and fluid source, fluid pathways, depositional mechanisms, and timing relative to regional structural and metamorphic events, continues to be controversial. However, there is now general agreement that these deposits formed from metamorphic fluids, either from metamorphism of intra-bas...
4 Citations Source Cite
2018 in Ore Geology ReviewsIF: 3.99
Liang Zhang3
Estimated H-index: 3
(China University of Geosciences),
Liqiang Yang21
Estimated H-index: 21
(China University of Geosciences)
+ 5 AuthorsJin-Song Peng
Abstract The Huangjindong gold deposit, with gold resources of ∼80 t, is hosted in Neoproterozoic slates along the Chang-Ping Fault in the Jiangnan Orogen, southern China. The orebodies are dominated by auriferous arsenopyrite-pyrite-quartz-(scheelite) veins; quartz-rich breccias that are cemented by late arsenopyrite, pyrite, muscovite, and quartz; auriferous stibnite-quartz veins; and disseminated gold in arsenopyrite-pyrite-sericite-quartz altered rocks. Neither significant alteration zoning ...
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2018 in Mineralium DepositaIF: 3.37
Hesen Zhao (China University of Geosciences), Qingfei Wang23
Estimated H-index: 23
(China University of Geosciences)
+ 1 AuthorsJun Deng29
Estimated H-index: 29
(China University of Geosciences)
The Danba gold deposit is located in a poorly-documented gold province on the north-western margin of the Yangtze Craton. It is sited in Devonian sequences in a high-grade metamorphic terrane that includes an extensional metamorphic core complex. Around the deposit, peak metamorphic conditions of 6 ± 0.5 kbar and 650 ± 50 °C at ca. 193 Ma were followed by retrograde sillimanite-grade conditions of 4.5 ± 0.5 kbar and 550 ± 50 °C. The deposit is hosted in a broadly strata-bound ductile-brittle she...
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2004
Richard J. Goldfarb3
Estimated H-index: 3
,
David I. Groves1
Estimated H-index: 1
+ 2 AuthorsRichard Vielreicher4
Estimated H-index: 4
1 Citations
1