Magmatism, metallogenic characteristics, and prospecting prediction for gold deposits in the north of Kunlun River area, Qinghai, China

JIAO He; KANG Jizu; HUANG Guobiao; JIA Jiantuan; PENG Jian; LU Haifeng; LEI Yanxiang

doi:10.12090/j.issn.1006-6616.2021159

Volume 28 Issue 3

Jun. 2022

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Article Navigation > Journal of Geomechanics > 2022 > 28(3): 383-405

JIAO He, KANG Jizu, HUANG Guobiao, et al., 2022. Magmatism, metallogenic characteristics, and prospecting prediction for gold deposits in the north of Kunlun River area, Qinghai, China. Journal of Geomechanics, 28 (3): 383-405. DOI: 10.12090/j.issn.1006-6616.2021159

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Magmatism, metallogenic characteristics, and prospecting prediction for gold deposits in the north of Kunlun River area, Qinghai, China

doi: 10.12090/j.issn.1006-6616.2021159

JIAO He^{1, 2
,},
KANG Jizu³,
HUANG Guobiao^{1, 2},
JIA Jiantuan^{1, 2},
PENG Jian^{1, 2
,
,},
LU Haifeng^{1, 2},
LEI Yanxiang^{1, 2}

1.
Qaidam Basin Comprehensive Geological and Mineral Exploration Institute of Qinghai Province, Golmud 816000, Qinghai, China
2.
Key Laboratory of Resource Exploration and Research, Qaidam Basin, Salt L., Golmud 816099, Qinghai, China
3.
Qinghai Provincial Geological Survey, Xining 810000, Qinghai, China

Funds:

the Geological Survey Project of China Geological Survey 1212011140113

More Information

Received: 2021-11-18
Revised: 2022-05-11

Abstract

Abstract

The north of Kunlun River area, which is close to the central Kunlun Fault Zone, has experienced multi-stage magmatic activities of early Paleozoic and Paleozoic-Mesozoic. A number of gold deposits (occurrences) have been discovered successively in this area for the past few years from west to east, such as Heihaibei, Lalingzaohuo, Suhaitu, Jiazutashixi, Xiangyanggou, Jiazutashidong, Dazaohuo and Heicigou, forming a metallogenic belt with an EW-length of nearly 150 km. In consideration of the basic characteristics of gold deposits in the belt, the ore-hosting wall rocks from the Heihaibei and Jiazutashidong gold deposits were selected to carry out zircon U-Pb dating in this study. The results show the silicified monzonitic granites from the Heihaibei deposit yield zircon weighted mean ²⁰⁶Pb/²³⁸U age of 443±8 Ma, which should be formed under the stretching environment after the collision of the Proto-Tethys Ocean to the Qaidam block. The diorite dikes from the Jiazutashidong deposit, which bears more inherited zircon, yield the zircon weighted mean ²⁰⁶Pb/²³⁸U age of 250±1 Ma and 420±2 Ma for primary zircon and inherited zircon, respectively, indicating a continental arc tectonic setting under the northward subduction of the Paleo-Tethys Ocean during the emplacement of diorites. Overall, it is believed that the gold mineralization in the northern Kunlun River area is more closely related to the Early Mesozoic Triassic magmatic activity, but opinions vary about the deposit types on whether it belongs to the orogenic or magmatic hydrothermal. Soil geochemical anomalies, low-resistance and high-polarization IP anomalies, and altered fracture zones formed by secondary faults can be used as the main ore prospecting markers in the northern of Kunlun River. It is considered that this metallogenic belt has good prospects for gold deposits.
- East Kunlun Orogen,
- north of Kunlun River area,
- magmatism,
- metallogenic characteristics of gold deposits,
- zircon U-Pb age

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