TY  - BOOK
AU  - Brodzikowski,Krzysztof
AU  - Loon,A.J.van
ED  - ScienceDirect eBooks.
TI  - Glacigenic sediments
T2  - Developments in sedimentology
SN  - 9780444883070
AV  - QE471.2 .B76 1991eb
PY  - 1991///
KW  - Sediments (Geology)
KW  - Glacial landforms
KW  - Glacial epoch
KW  - Drift (Glaciologie)
KW  - SCIENCE
KW  - Earth Sciences
KW  - Sedimentology & Stratigraphy
KW  - bisacsh
KW  - fast
KW  - Glaciale sedimenten
KW  - gtt
KW  - Electronic books
KW  - local
N1  - Includes bibliographical references and indexes; Preface. Introduction. General Characteristics of Glacigenic Sedimentation. The System of Glacigenic Depositional Environments. Glacigenic Facies and Their Characteristics. Tables of the Continental and Marine Glacigenic Environments, Subenvironments, Facies and Deposits. The Continental Supraglacial Subenvironment and its Deposits. The Continental Englacial Subenvironment and its Deposits. The Continental Subglacial Subenvironment and its Deposits. The Marine Glacial Environment and its Deposits. The Continental Terminoglacial Subenvironment and its Deposits. The Continental Proglacial Subenvironment and its Deposits. The Continental Extraglacial Subenvironment and its Deposits. The Marine Proglacial Subenvironment. The Marine Extraglacial Subenvironment and its Deposits. Epilogue. References. Subject Index.(Full contents available upon request to the publisher)
N2  - This book aims primarily at providing those involved in fundamental or applied research in the fields of geology, geomorphology and hydrology with a systematic overview of glacigenic sediments. A generally applicable terminology is proposed which should facilitate communication between scientists from several fields. Also it should form a bridge between western and eastern "schools" dealing with Quaternary geology. Because the book is mainly devoted to depositional processes and the resulting deposits, the approach and the terminology followed in this book are obviously founded strongly on sedimentology, the geological discipline that deals specifically with these phenomena. The book will be helpful in describing the sediments involved, interpreting their genesis, establishing their extent and their mutual relationships, and thus in the reconstruction of the palaeogeographic development. The large list of references reflects the author's extensive search of the literature
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ER  -