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[null,"1.","Record Nr.",null,"UNINA9910785066903321"]
[null,null,"Titolo",null,"A practical guide to the study of glacial sediments [[electronic resource] /] / edited by David J.A. Evans and Douglas I. Benn"]
[null,null,"Pubbl/distr/stampa",null,"London, : Arnold, 2004"]
[null,null,"ISBN",null,"0-203-78348-4"]
[{"$nulls":4},"1-282-66706-8"]
[{"$nulls":4},"9786612667060"]
[{"$nulls":4},"1-4441-1914-1"]
[null,null,"Descrizione fisica",null,"1 online resource (297 p.)"]
[null,null,"Disciplina",null,"551.79"]
[null,null,"Soggetti",null,"Drift"]
[{"$nulls":4},"Sedimentology"]
[{"$nulls":4},"Geology, Stratigraphic - Quaternary"]
[{"$nulls":4},"Geology - Fieldwork"]
[null,null,"Lingua di pubblicazione",null,"Inglese"]
[null,null,"Formato",null,"Materiale a stampa"]
[null,null,null,"Livello bibliografico","Monografia"]
[null,null,null,"Note generali","Description based upon print version of record."]
[null,null,null,"Nota di bibliografia","Includes bibliographical references and index."]
[null,null,"Nota di contenuto",null,"Cover; Book title; Contents; Preface; Acknowledgements; Figure Acknowledgements; Chapter 1 Introduction and rationale; Chapter 2 Facies description and the logging of sedimentary exposures; Chapter 3 The size of sedimentary particles; Chapter 4 Clast morphology; Chapter 5 Macrofabric; Chapter 6 Micro-scale features and structures; Chapter 7 Particle lithology (or mineral and geochemical analysis); Chapter 8 Engineering properties; Chapter 9 The research project - a case study of Quaternary glacial sediments; References; Index"]
[null,null,null,"Sommario/riassunto","Sediments are the most valuable form of physical evidence for past Earth surface processes. They have the potential to build up an archive of events and provide a window into the past. Through careful examination of sediments the shifting patterns of surface processes across space and time are revealed, allowing us to reconstruct past evironments and environmental change. A Practical Guide to the Study of Glacial Sediments is a guide to the standard techniques employed to read the sedimentary record of former glaciers and ice sheets. It demonstrates that the often complex and fragmentary glaci"]