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在右江地区海相层序地层学研究的基础上 ,将层序界面区分为升隆侵蚀层序不整合界面、海侵上超层序不整合界面、暴露层序不整合界面和造山侵蚀层序不整合界面四个成因类型 ,并且相同成因类型的层序界面 ,在盆内不同地域的具体表现形式不尽相同 ,它们与盆地的成生、发展有紧密的联系 ,这些界面类型依次反映了盆地的新生、演化和盆山转换过程
Based on the study of marine sequence stratigraphy in Youjiang area, the sequence boundaries are divided into uplift-erosion sequence unconformity interface, transgressive sequence-unconformity interface, exposure sequence unconformity interface and orogenic erosion layer Orderly and unconformity interfaces, and the sequence interfaces of the same genetic type have different manifestations in different regions of the basin. They are closely related to the genesis and development of the basin. These interface types reflect in turn Basin newborn, evolution and basin-mountain conversion process