Sedimentary Environments: Processes, Facies and Stratigraphy

sedimentary environments: processes, facies and stratigraphy

more information about Sedimentary Environments: Processes, Facies and Stratigraphy

Sedimentary Environments: Processes, Facies and Stratigraphy

Editorial Reviews
Book Description
Sedimentary Environments and Facies is one of the most distinguished and influential textbooks in the earth sciences published in the last twenty years. The two earlier editions won universal praise and became classic works in sedimentology Since the publication of the second edition, the study of sedimentary environments and facies has made great strides forward. There have been major advances in facies modelling, sequence stratigraphy and basin modelling. This dynamic stratigraphy lends a new element to the book; and the third edition should set a further benchmark and remain the textbook of choice for students in sedimentology.
Sedimentary Environments and Facies is one of the most distinguished and influential textbooks in the earth sciences published in the last twenty years. The two earlier editions won universal praise and became classic works in sedimentology Since the publication of the second edition, the study of sedimentary environments and facies has made great strides forward. There have been major advances in facies modelling, sequence stratigraphy and basin modelling. This dynamic stratigraphy lends a new element to the book; and the third edition should set a further benchmark and remain the textbook of choice for students in sedimentology.

Sedimentary Environments: Processes, Facies and Stratigraphy,Harold G. Reading,Blackwell Publishing, Incorporated,0632036273,Earth Sciences - Geology,Facies (Geology),Nuclear Physics,Rocks, Sedimentary,Science,Science/Mathematics,Sedimentary Geology,Sedimentary Rocks,Sedimentation and deposition,Environmental science,GEOLOGY, STRATIGRAPHIC,Geological surface processes (geomorphology),SEDIMENTARY STRUCTURES,SEDIMENTATION ANALYSIS,Science / Geology,Stratigraphy

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