1887

Abstract

The source of organic acids is commonly attributed to the early maturation of kerogen in source rocks. Organic acids are frequently interpreted as cause of burial related secondary porosity. Major deficiencies of this concept are insufficient oxygen in th

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/content/papers/10.3997/2214-4609.201400486
2009-06-08
2020-04-01
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400486
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