西南石油大学学报(自然科学版) ›› 2006, Vol. 28 ›› Issue (2): 11-15.DOI: 10.3863/j.issn.1000-2634.2006.02.004

• 地质勘探 • Previous Articles     Next Articles

DIAGENFSIS IN THE 2-SECTION OF JIALING.nANG OF THE TRANSITIIONED ZONE BETWEEN THE CENTER PART AND THE SOUTHERN PART OF SICHUAN BASINAND ITS EFFECT TO RESERVOIR DEVELOPMENT

ZHOU Yue-zong1 LEI Bian-jun1 ZHAO Yong-gang1 et al

  

  1. ( Southwest Petroleum University,Cheng-du Sichuan 610500, China)
  • Received:2005-12-23 Revised:1900-01-01 Online:2006-04-20 Published:2006-04-20
  • Contact: ZHOU Yue-zong

Abstract: The 2-section of Jialingjiang project belongs to strict and evaporated platform facies. Its main lithology is dolomite, gypsepus rock, limestone and a spot of pulpy rock. Arenite dolomite,politic dolomite, silty dolomite, silty-fine dolomite, politic lime-stone and arenite are of reservoir signification. The 2-section ofJiaLingjiang project has developed from seabed diagenesis,evaporated diagenesis, mixed water diagenesis, shallow-water,middle-water diagenesis environment and deep-water diagenesisenvironment. Early fresh-water leaching, near-surface(evaporating bump and refluent penetration)dolomitization, corrosion which is related to organic evolvement are the main member constructed diagenesis. The tectonic fracture has made its permea-
bility better. Besides, the compaction, pressolution,twice gypsum cementation are the 2-section of Jialingjiang project's main destructed diagenesis. The 2-section of Jialingjiang project has two types of studded carbonate rock and non-studded carbonate rock, which have 6 kind of lithology. This paper has created their diagenesis serial and the pore evolving mode.

Key words: diagenesis environment, pore evolution, section Ⅱof Jialingjiang Formation

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