1887

Abstract

The Upper Cretaceous Austin Chalk produces along the Gulf of Mexico coast, United<br>States, from secondary porosity and permeability created through fracturing. Several large fields,<br>including Giddings (222 MMBO, 76 BCF) and Pearsall (104 MMBO, 15 BCF) were developed<br>utilizing mostly vertical wells.

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/content/papers/10.3997/2214-4609.201407545
1994-09-09
2020-05-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407545
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