No. 7 Gold Geological Party

Yantai, China

No. 7 Gold Geological Party

Yantai, China

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Chen D.-X.,China University of Geosciences | Sun J.-G.,China University of Geosciences | Liu X.-H.,No. 7 Gold Geological Party | Lu S.-P.,No. 7 Gold Geological Party | And 2 more authors.
Northwestern Geology | Year: 2013

The outcrop of diabase dikes in Halaqi of Xinjiang has provided important information for tectonic evolution of southwest Tianshan area. The diabase dikes in Halaqi area lack HFSE (Nb, Ta) and HREE (Yb, Y), and exhibit enrichment in LILE (Ba, Sr, K) and LREE (La, Ce). With the geochemical characteristics of depleted mantle, it can be understood as the mantle was transformed by subduction in plate subduction, indicating that during the Late Carboniferous-Early Permian, the region should have been in the island arc environment.


Liu X.-H.,China University of Geosciences | Deng J.,China University of Geosciences | Sun X.-L.,China University of Geosciences | Liu J.-F.,No. 7 Gold Geological Party | And 2 more authors.
Jilin Daxue Xuebao (Diqiu Kexue Ban)/Journal of Jilin University (Earth Science Edition) | Year: 2010

The Ganbahenao deposit in the north Qilian Mountains is a middle Mo-W deposit newly discovered in the western segment of north Qilian Mountains. It belongs to the quartz vein type. Both molybdenite and wolframite are dominant metal minerals in the ore. Through the study of the geological features of the deposit, the C, H, O isotopic compositions of fluid inclusions in quartz and the content of both Re and S in molybdenite, authors conclude that ore-forming materials were derived from the crust, the ore-forming fluid mainly came from the magmatic fluid. The Ganbahenao deposit was genetically related to the S-type granite. Re-Os dating of molybdenite yields model ages between (413.3 ± 6.0)-(426.4 ± 6.6) Ma and an isochrone age of (424 ± 10) Ma, which is nearly equal to that of the wall rock, the Jinfosi S-type plutons. The Ganbahenao deposit and the Jinfosi plutons are formed in the environment of the continent-continent collision after the closure of the north Paleo-Qilian ocean in Late Silurian Period. The Jinfosi plutons offers the ore-forming sources and space.

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