--> Assessment and Enrichment Regulation of Global Oil Shale Resources
[First Hit]

2018 AAPG International Conference and Exhibition

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Assessment and Enrichment Regulation of Global Previous HitOilNext Hit Previous HitShaleNext Hit Resources

Abstract

Based on CNPC major science and technology programs research and many commercial database such as IHS, Robertson and C&C, this research established technologically recoverable coefficient by Previous HitoilNext Hit Previous HitshaleNext Hit, and evaluated the technical recoverable resource of the 31 global sedimentary basins by the volumetric method and analogy method. The results showed that the global Previous HitoilNext Hit Previous HitshaleNext Hit geological resources is 8345×108t, and the technical recoverable resources is 2099×108t. The global technical recoverable resources are mainly distributed in North America, Russia, Europe and South America, especially in the United States, Russia, Belarus, and Brazil. The largest four potential Previous HitoilNext Hit Previous HitshaleNext Hit formations are the Green River Previous HitshaleNext Hit in Piceance Basin, the Kashpir Previous HitshaleNext Hit in Ural-Volga Basin, the Mancos Previous HitshaleNext Hit in Uinta Basin and the Bazhenov Previous HitshaleNext Hit in West Siberian Basin. Foreland basin and craton basin are the favorable basin types for technical recoverable Previous HitoilNext Hit Previous HitshaleNext Hit resources. Also the technical recoverable Previous HitoilNext Hit Previous HitshaleNext Hit resources are rich in Jurassic, Cretaceous, Devonian, and Paleogene strata. The organic matter of Previous HitoilNext Hit Previous HitshaleNext Hit are mainly developed in lacustrine facies sedimentary environment, and most of the TOC abundance are between 8% - 15%, main type is given priority to with II1 type, closely followed by type I. Finally, the Previous HitoilNext Hit Previous HitshaleTop resources enrichment region have four typical characteristics: 1) a relatively stable tectonic conditions; 2) relative small hydrodynamic but deep water depth, 3) the climate with sufficient supply of source, and 4) the appropriate water condition.