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烃类形成、运移和聚集的常规研究实质上仅限于沉积盆地演化的埋藏过程,而其它地质作用,特别是与基底岩体的构造隆起和构造活动被完全忽视了。根据埋藏演化观念,反映源岩鼠熟和烃类形成的关键参数是温度,控制烃类排出祝运移的因素是上覆匠力对岩石的压实作用。根据这些前提,石油形成动力学研究的焦点是加热模拟实验有机质的成熟作用。而本模拟实验的目的是揭示构造变形对源岩的转化作用。
Conventional studies on the formation, migration and accumulation of hydrocarbons have been essentially limited to the burial process of sedimentary basin evolution, while other geological processes, especially structural tectonic uplift and tectonic activity, have been completely ignored. According to the concept of burial evolution, the key parameter that reflects the formation and evolution of hydrocarbons in the source rocks is the temperature. The key factor controlling hydrocarbon migration is the compaction of the overburden. Based on these premises, the focus of petroleum formation kinetics is to simulate the maturation of experimental organic matter. The purpose of this simulation experiment is to reveal the transformation effect of tectonic deformation on source rocks.