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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2008  >  30(6): 591-595
Zhang Linye. THE PROGRESS ON THE STUDY OF LACUSTRINE SOURCE ROCKS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2008, 30(6): 591-595. doi: 10.11781/sysydz200806591
Citation: Zhang Linye. THE PROGRESS ON THE STUDY OF LACUSTRINE SOURCE ROCKS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2008, 30(6): 591-595. doi: 10.11781/sysydz200806591
shu

THE PROGRESS ON THE STUDY OF LACUSTRINE SOURCE ROCKS

doi: 10.11781/sysydz200806591

  • Geological Scientific Research Institute, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257015, China

  • Received Date: 2008-07-01
  • Rev Recd Date: 2008-11-01
  • Publish Date: 2008-12-28
    Abstract
  • There is distinctive heterogeneity in the deposition of lacustrine source rocks.The occurrence of high-quality lacustrine source rocks with rich-organic matter plays an important role in controlling the formation of large oil fields.It has been widely concerned about the mechanism forming rich-organic matter in lacustrine source rock and has achieved significant advance.The deposition of high-quality source rocks has close relationships with the variation of the capacities of lacustrine basins during their evolution,paleolacustrine physicochemical properties,nutrition origin of paleo-productivity,periodic variation of climate and so on.In order to study the formation mechanism of high-quality source rocks,we should try to find out the dependence relations between organic compounds and inorganic elements in sedimentary rhythms in rich-organic matter strata,analyse the coupling relation between cyclicity and incident during geologic succession,inquire into the inherent connection among geologic environment,biogenetic derivation and the formation of rich-organic matter strata.

     

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