In this Book
Gulf of Mexico Origin, Waters, and Biota: Volume III, Geology
Book
2009
Published by:
Texas A&M University Press

summary
Volume 3 of Gulf of Mexico Origin, Waters, and Biota; a series edited by John W. Tunnell Jr., Darryl L. Felder, and Sylvia A. Earle
A continuation of the landmark scientific reference series from the Harte Research Institute for Gulf Of Mexico Studies, this volume provides the most up-to-date systematic, cohesive, and comprehensive description of the geology of the Gulf of Mexico basin. The book’s six sections address the Gulf’s origin (including petroleum resources), processes (including climate change), and coral reefs.
Knowledge about the foundation of the ocean environment remains vital to the understanding of the mineral and marine resources of the Gulf as well as the increasing effects of sedimentation and global warming. With this volume, much of the information necessary for a full view of the geology of the Gulf in the U.S., Mexico, and Cuba that was previously sequestered in the files of industry or government has been made more readily available for scientists, researchers, and students. It provides valuable synthesis and interpretation, representing nearly everything known about the geology of the Gulf of Mexico in the early twenty-first century.
Four years in the making, this monumental compilation is both a lasting record of the current state of knowledge and the starting point for a new millennium of study.
Table of Contents

pp. 141-154
pp. 157-173
pp. 175-193
pp. 195-208

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Download 12. Development of the Northwestern Gulf of Mexico Continental Shelf and Coastal Zone as a Result of the Late Pleistocene–Holocene Sea-Level Rise
- Save 12. Development of the Northwestern Gulf of Mexico Continental Shelf and Coastal Zone as a Result of the Late Pleistocene–Holocene Sea-Level Rise
pp. 209-228
pp. 279-290
pp. 367-379
pp. 381-390
ISBN | 9781603442930 |
---|---|
MARC Record | Download |
OCLC | 748104407 |
Pages | 512 |
Launched on MUSE | 2012-01-01 |
Language | English |
Open Access | No |