Clastic diagenesis has evolved from a very descriptive science to a much more process-oriented study. This evolution has been driven by the realization that many hydrocarbon reservoirs have significant diagenetic compotents directly affecting porosity and permeability characteristics. The prediction in time and space of reservoir characteristics affected by diagenesis can greatly reduce the risk in the search for hydrocarbon accumulations, particularly in subtle targets lacking pronounced structural expression. This publication contains three sections designed to increase understanding in the processes controlling clastic diagenesis: Conepts and Principles; Aspects of Porosity Modification; and Applications of Clastic Diagenesis in Exploration and Production. The first two sections deal with processes controlling various aspects of clastic diagenesis, and the third section applies these principles and observations to specific examples. Altogether, the three sections contain 22 chapters.
Diagenesis of Plio–Pleistocene Nonmarine Sandstones, Cagayan Basin, Philippines: Early Development of Secondary Porosity in Volcanic Sandstones
Published:January 01, 1984
Mark E. Mathisen, 1984. "Diagenesis of Plio–Pleistocene Nonmarine Sandstones, Cagayan Basin, Philippines: Early Development of Secondary Porosity in Volcanic Sandstones", Clastic Diagenesis, David A. McDonald, Ronald C. Surdam
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The Plio-Pleistocene nonmarine volcanic sandstones of the Cagayan basin, Philippines, have been significantly altered by early dissolution and cementation processes. The amount and type of alteration vary by formation, depth, and age of the deposit. Plio-Pleistocene fluvial sandstones (litharenites and feldspathic litharenites) buried to depths of 400–900 m, are only slightly compacted, but contain significant amounts of authigenic pore-lining clay and zeolites. Dissolution of plagioclase, heavy minerals, and volcanic rock fragments has occurred in nearly all samples, dissolving up to one-half the framework grains and increasing thin-section porosity to as much as 40%. The overlying Pleistocene sandstones are compositionally...