Genetic link between Mississippi Valley-type (MVT) Pb–Zn mineralization and hydrocarbon accumulation in the Niujiaotang ore field, SW China

Authors:
raw_author_name: Yong Cheng
raw_affiliation_string: Faculty of Land and Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China; Kunming Metallurgy College, Kunming 650033, China; School of Earth Sciences, Yunnan University, Kunming 650500, China
raw_author_name: Yuzhao Hu
raw_affiliation_string: Faculty of Land and Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China
raw_author_name: Jia-Xi Zhou
raw_affiliation_string: Key Laboratory of Critical Minerals Metallogeny in Universities of Yunnan Province, Kunming 650500, China; Key Laboratory of Sanjiang Metallization and Resource Exploration & Utilization, MNR, Kunming 650500, China; School of Earth Sciences, Yunnan University, Kunming 650500, China
raw_author_name: Shenjin Guan
raw_affiliation_string: Faculty of Land and Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China
raw_author_name: Saihua Xu
raw_affiliation_string: Faculty of Land and Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China
raw_author_name: Miao Cui
raw_affiliation_string: Panxi Geological Brigade of Sichuan Bureau of Geology and Mineral Resources, Xichang 615000, China
raw_author_name: Jinliang Zhang
raw_affiliation_string: Kunming Metallurgy College, Kunming 650033, China
raw_author_name: Xiaolin Tan
raw_affiliation_string: State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum (Beijing), Beijing 102249, China
raw_author_name: Liang Zhou
raw_affiliation_string: Department of Geology, Northwest University, Xi’an, Shaanxi 710069, China
raw_author_name: Zhennan Liu
raw_affiliation_string: Kunming Metallurgy College, Kunming 650033, China
raw_author_name: Kai Luo
raw_affiliation_string: Key Laboratory of Critical Minerals Metallogeny in Universities of Yunnan Province, Kunming 650500, China; Key Laboratory of Sanjiang Metallization and Resource Exploration & Utilization, MNR, Kunming 650500, China; School of Earth Sciences, Yunnan University, Kunming 650500, China
raw_author_name: Maoda Lu
raw_affiliation_string: 104 Geological Team, Guizhou Bureau of Geology and Mineral Exploration and Development, Duyun 558000, China

Abstract: The Niujiaotang MVT Pb-Zn ore field is located at the southwestern end of the West Hunan-East Guizhou (WHEG) metallogenic belt, which overlaps spatially with the Majiang paleo-oil reservoir. The Pb-Zn mineralization is closely associated with oil-gas accumulation processes. However, the genetic link between the paleo-oil reservoir and the Pb-Zn deposits remains unclear. In this paper, we present new findings of bitumen (paleo-oil reservoir) and its features in the deposits, and apply various isotopic geochemical methods and 2D seismic data to elucidate the source rock and coupling relationship of the paleo-oil reservoir and the Pb-Zn deposits. This study reveals that the ore has a simple mineral composition, mainly comprising sphalerite, pyrite, and dolomite. Solid bitumen occurs widely in the ore and the host dolostone, and coexists with minerals from the mineralization stage. Laser Raman spectroscopy shows that the bitumen in the wall rocks of the Chengong deposit and the Danzhai paleo-oil reservoir are both overmature, and their carbon isotope compositions (δ13CPDB = –29.17 ‰ – –31.20 ‰, average –30.10 ‰, n = 6) and initial 187Os/188Os ratio (1.08±0.19) suggest that they have the Lower Cambrian source rock similar to the Majiang paleo-oil reservoir. The δ34S value of pyrite in the bitumen from the wall rocks in the Chengong deposit ranges from +28.15 ‰ to +44.12 ‰ (average +33.28 ‰, n = 18), which is consistent with the sulfur isotope composition of the ore sulfide reported previously, indicating that they both derived from sulfate in the Middle-Upper Cambrian strata. Bitumen Re-Os and sphalerite Rb-Sr isotopic dating indicate that oil reservoir accumulation in the ore-hosting strata preceded Pb-Zn mineralization, occurring at 424±160 Ma (MSWD = 1.3) and 398±4.7 Ma (MSWD = 0.66), respectively. The initial 87Sr/86Sr ratio of sphalerite is 0.709983±0.000027, which, after comparison and in combination with previous studies, suggests that the metallogenic metals mainly originated from the underlying strata and basement. 2D seismic data show that the Zaolou fault (F2) that controls the mineralization is a deep fault that extends to the basin basement, and acts as a migration pathway for hydrocarbon fluids and ore-forming materials. We propose that liquid hydrocarbons played a significant role in Pb-Zn mineralization, acting as reductants to reduce sulfate through the thermochemical sulfate reduction (TSR) reaction and provide abundant reduced sulfur (H2S/HS−) for Pb-Zn mineralization. Finally, we present a comprehensive model of hydrocarbon accumulation and mineralization in the Niujiaotang ore field.