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首页> 外文期刊>Journal of Asian earth sciences >Lower limit of hydrocarbon generation in source rocks: A case study from the Dongpu Depression, Bohai Bay Basin, East China
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Lower limit of hydrocarbon generation in source rocks: A case study from the Dongpu Depression, Bohai Bay Basin, East China

机译:烃源岩生烃的下限:以中国东部渤海湾盆地东圃De陷为例

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摘要

With the increasing demand for hydrocarbons, exploration tends to be deeper and unconventional resources. However, whether there are the lower limits for exploration depth or thermal maturity (R-o) appears to be particularly essential. It is of considerable significance to determine the lower limit of hydrocarbon generation (LLHG) since this limit can provide guidelines for hydrocarbon potential estimation. According to the mechanisms of hydrocarbon generation and expulsion, five methods are combined to determine and verify the LLHG, whose values can be expressed by LLHG((Ro)) ( )and LLHG((H)). Source rock samples from the Paleogene Shahejie Formation (Es) in the Dongpu Depression were taken as an example to determine the LLHG, and then controlling factors of the LLHG were discussed. LLHG((Ro)) values for Es range from 3.23% to 3.97% (average 3.71%) and LLHG((H)) values range from 5244 m to 5525 in (average 5433 m). Regionally, LLHG values display obvious differences between the northern and southern of depression. LLHG values in the north are roughly larger than those in the south. In the northern depression, the LLHG(()(Ro)()) values are ranging from 3.61% to 3.97% (average 3.81%) and LLHG((H) )values are ranging from 5415 m to 5545 m (average 5488 m). However, in the southern part, the LLHG((Ro)) values range from 3.20% to 3.74% (average 3.48%) and the LLHG((Ro)) values range from 5265 m to 5375 in (average 5278 m). The main controlling factors for LLHG diversity between the north and the south of depression are organic matter (OM) type and abundance, formation temperature and pressure.
机译:随着对碳氢化合物需求的增加,勘探趋向于成为更深层的非常规资源。但是,对于勘探深度或热成熟度(R-o)是否有下限显得尤为重要。确定碳氢化合物生成量的下限(LLHG)具有相当重要的意义,因为该上限可以为估算碳氢化合物潜力提供指导。根据生烃和驱出的机理,结合了五种方法来确定和验证LLHG,其值可以用LLHG((Ro))()和LLHG((H))表示。以东圃De陷古近系沙河街组(Es)的烃源岩样品为例,确定了LLHG,然后讨论了LLHG的控制因素。 Es的LLHG((Ro))值范围为3.23%至3.97%(平均3.71%),LLHG((H))值范围为5244 m至5525 in(平均5433 m)。在区域上,LLHG值在凹陷北部和南部之间显示出明显的差异。北部的LLHG值大致大于南部的LLHG值。在北部洼地,LLHG((Ro)())值范围从3.61%到3.97%(平均3.81%),LLHG((H))值范围从5415 m到5545 m(平均5488 m) )。但是,在南部,LLHG((Ro))值的范围为3.20%至3.74%(平均3.48%),LLHG((Ro))值的范围为5265 m至5375 in(平均5278 m)。凹陷北部和南部之间LLHG多样性的主要控制因素是有机质(OM)类型和丰度,地层温度和压力。

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