Skip to main content
Journal Article

Depositional facies, diagenetic terranes and porosity development in Lower Ordovician Ellenburger Dolomite, Puckett Field, west Texas.

Carbonate Petroleum Reservoirs (1986) 19-37
DOI: 10.1007/978-1-4612-5040-1_2
N/ACitations
Citations of this article
17Readers
Mendeley users who have this article in their library.
Get full text

Abstract

Puckett Field produces gas and gas condensate from structurally entrapped reservoirs in porous Ordovician dolomite. Porosity occurs as solution-collapse breccia and intercrystalline porosity interconnected by fracture porosity. Shales appear to form the major seal for trapped hydrocarbons.-R.A.H.

Cite

CITATION STYLE

APA

Loucks, R. G., & Anderson, J. H. (1986). Depositional facies, diagenetic terranes and porosity development in Lower Ordovician Ellenburger Dolomite, Puckett Field, west Texas. Carbonate Petroleum Reservoirs, 19–37. https://doi.org/10.1007/978-1-4612-5040-1_2

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free