About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

AAPG Bulletin

Abstract


Volume: 44 (1960)

Issue: 6. (June)

First Page: 961

Last Page: 961

Title: Facies and Porosity Relationship in Some Mississippian Carbonate Cycles of Western Canada Basin: ABSTRACT

Author(s): G. E. Thomas, R. P. Glaister

Article Type: Meeting abstract

Abstract:

Case histories of textural and reservoir analyses of selected Mississippian carbonate cycles of the Western Canada Basin are presented to illustrate the relationship that exists between the occurrence and petrographic nature of an Previous HiteffectiveNext Hit carbonate reservoir rock and the framework of carbonate sedimentation. Various types of carbonate rock pores are described and evaluated with respect to Previous HiteffectiveNext Hit porosity.

Large stratigraphic oil pools have been discovered, at or near the Paleozoic subcrop of the Mississippian "Midale" carbonate cycle, in southeastern Saskatchewan. Apart from scattered, vuggy, algal-encrusted strand line deposits, most of the carbonates of the "Midale" producing zone consist of skeletal and oolitic limestones which have a finely comminuted, frequently dolomitized, limestone matrix with intergranular and chalky porosity. Previous HitEffectiveNext Hit reservoir porosity is controlled by the relative distribution and grain size of this matrix.

Major hydrocarbon (oil and gas) reserves have been found in the Mississippian "Elkton" carbonate cycle, both in the Foothills Belt and along the subcrop, in southwestern Alberta. Previous HitEffectiveTop reservoir material of this cycle was found to consist mainly of the dolomitized equivalent of an originally coarse skeletal limestone, with a variable amount of generally porous, finely comminuted (granular) skeletal matrix. Primary porosity was very important in the control of dolomitization which probably began with the replacement of this matrix by euhedral rhombohedrons and finally affected the coarse skeletal material (now generally indicated by leached fossil cast outlines). These porous dolomites grade laterally in a predictable way into tight, relatively undolomitized, well sorted, coarse sk letal limestones with original high interfragmental porosity now completely infilled with clear crystalline calcite. This lithification by cementation took place early in the history of carbonate sedimentation of this area and before secondary dolomitization processes took effect.

End_of_Article - Last_Page 961------------

Copyright 1997 American Association of Petroleum Geologists