Abstract
The Qinshui Basin is in the Central Orogenic Belt of the North China Craton (NCC), and the production of coalbed methane accounts for 70% of China’s total coalbed methane output. Aiming at the unclear dynamic causes of large-scale coalbed methane accumulation in the basin and the unclear response relationship with the destruction of the NCC, we present joint illite crystallinity and vitrinite reflectance study across the Zijin Mountain and Qincan 1 wells of the Qinshui Basin, respectively. Inverse modeling suggested that tectono-thermal events occurred during the Early Cretaceous, associated with the maximum burial depth and heat flow. The maximum paleo-geothermal temperature and gradient reconstruction results recorded at the Carboniferous strata are 180–190°C and 6.5°C/100 m. The denudation thicknesses recorded by illite crystallinity of Zijinshan and the vitrinite reflectance of the Qincan 1 Well are 3,180.63 m and 3,269.32 m, respectively. We propose that the Qinshui Basin was affected by the extensional environment of the NCC, which caused deep lithospheric thinning and magma upwelling, and a tectono-thermal event occurred during the Early Cretaceous in Qinshui Basin. In addition, the accumulation of coalbed methane, triggered by a tectono-thermal event during the Early Cretaceous, is consistent with the early Cretaceous accumulation and mineralization events in the NCC. Overall, our results reflect the subduction event influence of the western Pacific plate into the East Asian continental plate on the tectono-thermal history of the Central Orogenic Belt of the NCC, which is theoretically significant for clarifying the thermal lithospheric thickness and rheological structure of the basin, as well as the evolutionary history of coalbed methane, and the basin response relationship to the destruction of the NCC.
Highlights
The Qinshui Basin belongs to the Shanxi block in the center of the North China Craton (NCC) (He, 2015; Zhu et al, 2015)
The clay minerals in the Triassic, Jurassic, Permian, and Cambrian strata in the central area of the Qinshui Basin are dominated by illite, and the combination of clay minerals is I + C + K
The clay mineral assemblage in the Carboniferous strata is dominated by kaolinite, and the clay mineral assemblage is I + C + K with the high interlayer ratio of I/S disorder, and illite accounts for 80–90% (Figure 4; Figure 5A)
Summary
The Qinshui Basin belongs to the Shanxi block in the center of the North China Craton (NCC) (He, 2015; Zhu et al, 2015). It is one of the areas with the most abundant coal resources within the NCC, and the production of coalbed methane ranks first in China. Tectono-Thermal History of Qingshui Basin, NCC of coalbed methane drilling wells in China, making it one of China’s most important energy sources (Zhao et al, 2016; Li Z. et al, 2018, Li et al, 2018 R.). Additional evidence shows that the lithospheric thickness in the central and western parts of the NCC varies greatly (Chen, 2009; Chang et al, 2011; Ling et al, 2017), indicating that the thinning and reformation of the lithospheric mantle occurred in the central and western NCC, but the influence of destruction event on the Qinshui Basin remains unclear
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