论文部分内容阅读
通过对“古龙凹陷青山口组泥岩裂缝成因机理”的研究，认为青山口组泥岩裂缝是成岩作用和异常高压共同作用的结果。较详细地探讨了青山口组泥岩异常高压裂缝的形成及其在目前地层条件下所保持的状态。
Through the research on the genesis mechanism of shale cracks in Qingshankou Formation in Gulong Sag, it is considered that the shale cracks in Qingshankou Formation are the result of the combination of diagenesis and abnormal pressure. The formation of abnormally high pressure fractures of mudstone in Qingshankou Formation and their status under the current formation conditions are discussed in more detail.