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The AAPG/Datapages Combined Publications Database

Houston Geological Society Bulletin

Abstract


Houston Geological Society Bulletin, Volume 52, No. 9, May 18, 2010. Page 19-19.

Abstract: Granite to Grass Roots: Understanding the Geologic History of Previous HitUnconventionalNext Hit Resource Basins from Bottom to Top

Harris Cander
BP America Houston, Texas

The competition for Previous HitunconventionalNext Hit resources in North America has resulted, in some cases, in the acquisition of acreage prior to obtaining an understanding of Previous HitsubsurfaceNext Hit technical risks or identification of fairway boundaries and sweet spots. Indeed, the term “resource play” implies to some that Previous HitsubsurfaceNext Hit risks are either minimized or irreducible. As well, the term “Previous HitunconventionalNext Hit gas” connotes that little is to be gained from application of conventional principles of basin evolution and petroleum generation, migration, and entrapment. Under these circumstances, the value of regional geologic understanding of an entire basin prior to acreage capture can be overlooked and the focus turned to completions technology and post-well analysis.

This lecture will discuss the importance of understanding a basin from basement to surface – granite to grass roots – in the search for Previous HitunconventionalNext Hit fairways. The lecture will include a holistic Previous HitintegrationNext Hit of Previous HitdataNext Hit and interpretations from basin modeling, petroleum migration modeling, gas isotope Previous HitdataNext Hit, pressure history, seismic, and reservoir quality. Linkages will be made from microscopic scale observations to tectonic-scale processes. Examples will be given from various North American basins that illustrate how mega-scale features, such as basement architecture and Precambrian rift history, have a first order and transcendent effect on the evolution and occurrence of Previous HitunconventionalTop resource fairways, including a strong influence on petroleum generation and entrapment as well as changes in reservoir rock during post-orogenic uplift.

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