Regional Geology and Tectonics : Phanerozoic Rift Systems and Sedimentary Basins

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Material type:

TextLanguage: English Series: ; 2 v.Publication details: Amsterdam : Elsevier , 2012 .Description: xxxviii,528pISBN:

9780444563569

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Other classification:

H23 Q2 TH

Summary: Regional Geology and Tectonics: Phanerozoic Rift Systems and Sedimentary Basins, volume two in a three-volume series covering Phanerozoic regional geology and tectonics. Experience in analyzing and assessing rifts―locations where the Earth’s outer shell and crust have been stretched over time by seismic activity―is critical for you as an exploration geologist in identifying Earth’s most lucrative hydrocarbon locations in which extraction is both efficient and safe. Vast compilations of related industry data present regional seismic lines and cross sections, and summaries of analogue and theoretical models are provided as an essential backdrop to the structure and stratigraphy of various geological settings.

Item type:

Textbook

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Holdings
Cover image	Item type	Current library	Home library	Collection	Shelving location	Call number	Materials specified	Vol info	URL	Copy number	Status	Notes	Date due	Barcode	Item holds	Item hold queue priority	Course reserves
	Textbook	Central Science Library	Central Science Library			H23 Q2 TH (Browse shelf(Opens below))		1B			Available			SL1558571

Includes bibliographical references.; Index 509-528p.

Regional Geology and Tectonics: Phanerozoic Rift Systems and Sedimentary Basins, volume two in a three-volume series covering Phanerozoic regional geology and tectonics. Experience in analyzing and assessing rifts―locations where the Earth’s outer shell and crust have been stretched over time by seismic activity―is critical for you as an exploration geologist in identifying Earth’s most lucrative hydrocarbon locations in which extraction is both efficient and safe. Vast compilations of related industry data present regional seismic lines and cross sections, and summaries of analogue and theoretical models are provided as an essential backdrop to the structure and stratigraphy of various geological settings.

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