Ordovician and Silurian Rocks of the Michigan Basin and Its Margins
Author: Karen Rose Cercone
Publisher:
Published: 1985
Total Pages: 204
ISBN-13:
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Author: Karen Rose Cercone
Publisher:
Published: 1985
Total Pages: 204
ISBN-13:
DOWNLOAD EBOOKAuthor: Paul A. Catacosinos
Publisher: Geological Society of America
Published: 1991
Total Pages: 258
ISBN-13: 081372256X
DOWNLOAD EBOOKAuthor: G. Michael Grammer
Publisher: Geological Society of America
Published: 2018-04-12
Total Pages: 350
ISBN-13: 0813725313
DOWNLOAD EBOOKThe Michigan Basin is a classic intracratonic basin that has played a significant role in the fundamental understanding of geological processes in such basins, and has been an important resource for oil and gas, economic minerals, groundwater, and coal. Despite the classic nature of the Michigan Basin, there has not been a "special volume" dedicated to the basin in nearly 25 years. Since that time, new advancements in the geological sciences, particularly the utilization of high-resolution sequence stratigraphy and three-dimensional geostatistical modeling, have led to a new and more comprehensive understanding of the Paleozoic sedimentary packages of the Michigan Basin. This volume provides significant new insights of the Michigan Basin to both academic and applied geoscientists; it includes papers that discuss various aspects of the sedimentology and stratigraphy of key units within the basin, as well as papers that analyze the diverse distribution of natural resources present in this basin.
Author: Brian J. Witzke
Publisher: Geological Society of America
Published: 1996-01-01
Total Pages: 453
ISBN-13: 081372306X
DOWNLOAD EBOOKAuthor: Andrea Förster
Publisher: Springer Science & Business Media
Published: 2012-12-06
Total Pages: 250
ISBN-13: 1461547512
DOWNLOAD EBOOKGeothermics in Basin Analysis focuses on the study of sedimentary basins, stressing essential parts of problems in which geothermics is involved. Subject matter includes the measuring of temperature logs and capturing of industrial temperature data and their interpretation to delineate subsurface conditions and processes, the importance of porosity and pore filling for modeling thermal fields, the thermal insulation of shales, geothermal anomalies associated with mud diapirs and basin hydrodynamic regimes, temperatures related to magmatic underplating and plate tectonics.
Author: Paul A. Catacosinos
Publisher:
Published: 2001
Total Pages: 62
ISBN-13:
DOWNLOAD EBOOKAuthor: John K. Warren
Publisher: Springer Science & Business Media
Published: 2006-06-12
Total Pages: 1042
ISBN-13: 3540323449
DOWNLOAD EBOOKComprehensive discussion of the role of evaporites in hydrocarbon generation and trapping Excellent introduction in the field
Author: Brian J. Witzke
Publisher:
Published: 1992
Total Pages: 120
ISBN-13:
DOWNLOAD EBOOKAuthor: John A. Rupp
Publisher:
Published: 1991
Total Pages: 116
ISBN-13:
DOWNLOAD EBOOKAuthor: John K. Warren
Publisher: Springer
Published: 2016-05-18
Total Pages: 1822
ISBN-13: 3319135120
DOWNLOAD EBOOKThe monograph offers a comprehensive discussion of the role of evaporites in hydrocarbon generation and trapping, and new information on low temperature and high temperature ores. It also provides a wealth of information on exploitable salts, in a comprehensive volume has been assembled and organized to provide quick access to relevant information on all matters related to evaporites and associated brines. In addition, there are summaries of evaporite karst hazards, exploitative methods and problems that can arise in dealing with evaporites in conventional and solution mining. This second edition has been revised and extended, with three new chapters focusing on ore minerals in different temperature settings and a chapter on meta-evaporites. Written by a field specialist in research and exploration, the book presents a comprehensive overview of the realms of low- and high-temperature evaporite evolution. It is aimed at earth science professionals, sedimentologists, oil and gas explorers, mining geologists as well as environmental geologists.