Abstract:
ObjectiveThe organic-rich shales of the Lower Cambrian in South China are characterized by significant thickness and high thermal maturity. Recent explorations have yielded industrial gas flows from the Lower Cambrian shales in the Middle Yangtze region. To further investigate the shale gas resource potential of the Lower Cambrian in South China, this study focuses on the Lower Cambrian Shuijingtuo Formation in the Middle Yangtze region.
MethodsThrough an integrated analysis of outcrop observations and drilling data, we analyzed its sedimentary characteristics and processes. A third-order stratigraphic sequence framework for the Lower Cambrian shale was established, and a sedimentary model of the Early Cambrian E’Xi Trough in the Middle Yangtze region was constructed, clarifying exploration targets.
ResultsThe Lower Cambrian Shuijingtuo Formation in the Middle Yangtze region primarily consists of shallow-water and deep-water shelf facies, with shallow carbonate deposits at both the bottom and top. The Lower Cambrian organic-rich shales can be divided into five third-order sequences, which are correlatable with those in the Upper Yangtze region. The Shuijingtuo Formation formed during the filling stage of the E’xi Trough, primarily consisting of argillaceous clastic sedimentary rocks.
ConclusionOrganic-rich shales are distributed in deep-water facies, with two identified subsags within the E’xi Trough (the Enshi and Yichang–Changyang depressions) serving as key exploration targets. The Lower Cambrian Shuijingtuo Formation, together with the underlying Sinian Dengying and Doushantuo Formations, forms a "sandwich-like" conventional hydrocarbon assemblage, which is a priority area for future conventional oil and gas exploration in Western Hubei.