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油气形成与南华山、西华山推覆体

Controlling Factors of Oil and Gas in South and West Hua Mountains
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摘要 厚达3200m的南华山、西华山冲断席掩覆在白垩系之上,使白垩系生油层埋深4400m,进入生油门限。生油层之上始新统寺口子组砂岩是理想的储集层;渐新统清水营组泥岩石膏层是很好的盖层。寻找掩伏体中生界的构造圈闭是本区找油的关键。 South Hua mountain and West Hua mountain located in the northwest margin of Liupanshan Basin: Haiyuan County. Ningxia. The strata developed there are lacustrine deposits, organic- riched dark mudstone of lower Cretaceous with a thickness of from 200m to 800m. The overlying strata are sandstone rudyte of Sikouzi formation (E25); and mudstone. gypsum layers of Qingshuiying formation IE39) .The strata are ideal assemblages of source rock, reservoir and cap for oil. but commercial oil has not been found.Based on the analysis of samples and TTI calculations, the burial depth of oil-generating strata is not deep enough to reach the oil forming threshold. It was reported in 1986 that South and West Hua mourtains are the northeastern uprakss of nappe structure in Qilianshan fold belt. The mountains as a overthrust sheet, which's thickness is more than 3200m, upthrusted on the oil-generating strata and made the burial depth enlarged then the condition of temperature increasing is available and oil-generating threshold can be got into. Moreover, overthrust belt led to the formation of special oil and gas pool.The key work of this region is searching for structural traps under nappe structure by the aid of physical survey.
作者 邓云山
出处 《沉积学报》 CAS CSCD 北大核心 1991年第1期122-128,共7页 Acta Sedimentologica Sinica
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参考文献2

  • 1张伯声,西北大学学报,1975年,3期
  • 2关士聪,地质知识,1957年,2期

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