石油与天然气地质 ›› 1991, Vol. 12 ›› Issue (1): 1-9.doi: 10.11743/ogg19910101

• 论文 •    下一篇

松辽盆地北部下白垩统下部含浊沸石砂岩的成岩作用

杨宝星1, 林仲虔1, 古世祥2   

  1. 1. 成都地质学院;
    2. 大庆石油管理局
  • 收稿日期:1989-06-20 修回日期:1990-02-28 出版日期:1991-03-25 发布日期:2012-01-16

DIAGENESIS OF LAUMONTITE-BEARING SANDSTONES IN LOWER PART OF LOWER CRETACEOUS,NORTH SONGLIAO BASIN

Yang Baoxing1, Lin Zhongqian1, Gu Shixiang2   

  1. 1. Chengdu College of Geology;
    2. Daqing Petroleum Administration
  • Received:1989-06-20 Revised:1990-02-28 Online:1991-03-25 Published:2012-01-16

PDF (PC)

424

被引次数

20

摘要：

松辽盆地北部深层下白垩统的砂岩为成分成熟度很低的岩屑长石砂岩及长石岩屑砂岩。主要成岩作用有:自生粘土边、石英长石次生加大、斜长石的钠长石化、自生浊沸石,以及次生长石和浊沸石溶蚀等。斜长石的钠长石化作用是浊沸石析出的主要机制,而粘土矿物的转化则为浊沸石的沉淀提供了钠和硅的来源。

关键词: 松辽盆地, 砂岩, 成岩作用, 浊沸石

Abstract:

Deep buried sandstones of Lower Cretaceous in North Songliao Basin are compositionally immature lithic arkose and feldspathic litharenite. The main diagenesis of the sandstones includes:authigenetic clay rim, quartz and feldspar overgrowth, albitization,authigenetic laumontite and the dissolution of feldspar and laumontite. The albitization of anorthosite is the primary mechanism for generating laumontite, whereas the transformation of clay minerals provides sodium and silicon for the precipitation of laumontite.