一维盆地模拟系统 BAS1,已在微机、VAX 和 IBM 机上研制成功,并成功地应用于临清坳陷东部和泌阳凹陷的资源评价。BAS1系统是在既吸收国际上某些先进模型、又独创一些模型的基础上建成的,包括四个模型:地史,热史,生烃史,排烃史。输入资...一维盆地模拟系统 BAS1,已在微机、VAX 和 IBM 机上研制成功,并成功地应用于临清坳陷东部和泌阳凹陷的资源评价。BAS1系统是在既吸收国际上某些先进模型、又独创一些模型的基础上建成的,包括四个模型:地史,热史,生烃史,排烃史。输入资料主要来自于地质、测井、地震和地化。输出结果是盆地的沉积史、构造史、古热流史、古地温史、R。史、TTI 史、生烃史和排烃史。同时,三维盆地模拟系统 BAS3已在 IBM 和 VAX机上初步研制成功,即将投入应用。本文仅介绍 BAS1系统及其在临清坳陷东部和泌阳凹陷的应用效果。展开更多
Base-level is a kind of surface which controls sedimentation and erosion. So, it can be concluded that it is base-level change that controls the formation and internal structure of a sequence. A single cycle of base-l...Base-level is a kind of surface which controls sedimentation and erosion. So, it can be concluded that it is base-level change that controls the formation and internal structure of a sequence. A single cycle of base-level change can generate four sets of different stacking patterns. They are two sets of aggradation, one progradation and one retrogradation, which affects the features of the internal structure of a sequence. Lishu fault subsidence of Songliao basin is a typical half-graben lacustrine basin. Comprehensive base-level change analysis indicates that six base-level cycles and their related six sequences can be recognized between T 4 and T 5 seismic reflection surface. The contemporaneous fault is the main controlling factor of the fault lacustrine basin. There are obvious differences exist in the composition of sedimentary systems and all systems tracts between its steep slope (the side that basin control fault existed) and flat slope. Except highstand systems tract is composed of fan delta-lacustrine system, lowstand systems tract, transgressive systems tract and regressive systems tract are all made up of fan delta-underwater fan-lacustrine sedimentary systems in the side of steep slope.展开更多
文摘Base-level is a kind of surface which controls sedimentation and erosion. So, it can be concluded that it is base-level change that controls the formation and internal structure of a sequence. A single cycle of base-level change can generate four sets of different stacking patterns. They are two sets of aggradation, one progradation and one retrogradation, which affects the features of the internal structure of a sequence. Lishu fault subsidence of Songliao basin is a typical half-graben lacustrine basin. Comprehensive base-level change analysis indicates that six base-level cycles and their related six sequences can be recognized between T 4 and T 5 seismic reflection surface. The contemporaneous fault is the main controlling factor of the fault lacustrine basin. There are obvious differences exist in the composition of sedimentary systems and all systems tracts between its steep slope (the side that basin control fault existed) and flat slope. Except highstand systems tract is composed of fan delta-lacustrine system, lowstand systems tract, transgressive systems tract and regressive systems tract are all made up of fan delta-underwater fan-lacustrine sedimentary systems in the side of steep slope.
