On The Microscopic Patterns Of The Continental Hydrocarbon Source Rock Organic Matter

Through rock sheet and Baofen residues observation, Jiyang Aoxian of three ofhydrocarbon source rock organic Fucun There are two main ways: standConcentrations and scattered organic matter. Stand Concentrations organic body wasdivided into algal scrap stand Concentrations of organic and non-stereotypedgroup-based stand Concentrations matter, the latter is subdivided into: Concentrationsof particulate organic matter and networking Concentrations. Concentrations aredivided into local populations scattered and dispersed organic matter categories.Layered concentrates the organic matter to come from the lasting lamination lakeand the season lamination lake, as well as the high lake biology production rate, thealgae thrive in turn, the organic matter pulse type fast deposition and the first floorwater oxygen deficit strongly restore the environment; Partial concentrates the organicmatter also to request the high lake biology production rate, but the lasting fastdeposition, the deposit has not elected continuously after the full minute possibly isthe main origin factor, or, primitively becomes the level to concentrate the organicmatter to mix by the intense biology the destruction also is one of important attributes;The dispersed organic matter produces from the biological production rate lowoxidation environment.Enriched material originating from the main stand muddy rock type designsstand, located in group study Kong shop, sand four, and three of sand, sand on the eastand south stratum layer spaces stability; Can be seen in the scattered populations ofthe various layers of the three departments, and non-profile stand muddy rock type.Horizontal, stand Concentrations matter distribution in the semi-deep lake in adeep lake, scattered populations located in shore-shallow lake videos, localConcentrations organic borderline.