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Late Cenozoic Evaporite Tectonism and Volcanism in West-Central Colorado (Geological Society of America Special Paper) - Softcover
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- PublisherGeological Society of Amer
- Publication date2002
- ISBN 10 0813723663
- ISBN 13 9780813723662
- BindingPaperback
- LanguageEnglish
- Number of pages234
- EditorKirkham Robert M., Scott Robert B., Judkins Thomas W.
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Late Cenozoic Evaporite Tectonism and Volcanism in West-Central Colorado
Published by
Geological Society of America, 2002
ISBN 10: 0813723663
ISBN 13: 9780813723662
Used
Hardcover
Seller: ThriftBooks-Atlanta, AUSTELL, GA, U.S.A.
Seller rating 5 out of 5 stars
Hardcover. Condition: Very Good. No Jacket. May have limited writing in cover pages. Pages are unmarked. ~ ThriftBooks: Read More, Spend Less 1.55. Seller Inventory # G0813723663I4N00
Quantity: 1 available
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Late Cenozoic Evaporite Tectonism and Volcanism in West-Central Colorado
Published by
Boulder, CO The Geological Society of America, 2002
ISBN 10: 0813723663
ISBN 13: 9780813723662
Used
Soft cover
First Edition
Seller: Jeff Jeremias Fine Arts, RMABA, Aurora, CO, U.S.A.
Seller rating 5 out of 5 stars
Soft cover. Condition: Fine. 1st Edition. First edition. 234 pages. Filled with black and white photos, charts and diagrams. Fine throughout. (B6). Seller Inventory # 4346
Quantity: 1 available
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Late Cenozoic Evaporite Tectonism and Volcanism in West-Central Colorado (Geological Society of America Special Paper)
Published by
Boulder, Colorado, USA : The Geological Society of America, 2002
ISBN 10: 0813723663
ISBN 13: 9780813723662
New
Soft cover
Seller: Joseph Burridge Books, London, United Kingdom
Seller rating 5 out of 5 stars
Soft cover. Condition: New. Regional late Cenozoic evaporite tectonism has caused widespread collapse in west-central Colorado. Miocene volcanic rocks are downdropped as much as 1200 m in a collapsed area that is at least 3600 km2 and possibly more than 5000 km2. During the late Cenozoic, rivers removed an estimated 2300 km3 of dissolved evaporite from the contiguous Carbondale and Eagle collapse centers. Collapse was quantified by restoration of deformed Miocene to Quaternary basaltic flows to their pre-collapse position. Late Cenozoic incision rates increased by an order of magnitude during the past 3 m.y., probably triggering or accelerating diapirism and dissolution of evaporite. Annual dissolved solids loads in rivers indicate that removal of evaporite continues at a rate that matches independent geologic estimates. Seller Inventory # PGGEO185
Quantity: 1 available