000 02481cam a22002894a 4500
001 11029
003 IN-BhIIT
005 20240627111957.0
008 100604s2011 enka b 001 0 eng
020 _a9788126560165
040 _aIN-BhIIT
041 _aeng
082 0 0 _a552.5
_bLEE/S
100 1 _aLeeder, M. R.
_eAuthor
_923588
245 1 0 _aSedimentology and sedimentary basins :
_bfrom turbulence to tectonics /
_cby Mike Leeder.
250 _a2nd ed.
260 _aNew Delhi :
_bWiley-Blackwell,
_c2016.
300 _axiii, 768 p. :
_bill. ;
_c26 cm.
500 _aMachine generated contents note: Contents list will be adapted from contents of current edition based on recommendations of reviewers.
504 _aIncludes bibliographical references and index.
505 8 _aMachine generated contents note: Contents list will be adapted from contents of current edition based on recommendations of reviewers.
520 _a"The sedimentary record on Earth stretches back more than 4.3 billion years and is present in more abbreviated forms on companion planets of the Solar System, like Mars and Venus, and doubtless elsewhere. Reading such planetary archives correctly requires intimate knowledge of modern sedimentary processes acting within the framework provided by tectonics, climate and sea or lake level variations. The subject of sedimentology thus encompasses the origins, transport and deposition of mineral sediment on planetary surfaces. The author addresses the principles of the subject from the viewpoint of modern processes, emphasising a general science narrative approach in the main text, with quantitative background derived in enabling 'cookie' appendices. The book ends with an innovative chapter dealing with how sedimentology is currently informing a variety of cognate disciplines, from the timing and extent tectonic uplift to variations in palaeoclimate. Each chapter concludes with a detailed guide to key further reading leading to a large bibliography of over 2500 entries. The book is designed to reach an audience of senior undergraduate and graduate students and interested academic and industry professionals."--
520 _a"The sedimentary record on Earth stretches back more than 4.3 billion years and is present in more abbreviated forms on companion planets of the Solar System, like Mars and Venus, and doubtless elsewhere"--
650 0 _aSedimentology.
_99150
650 0 _aSedimentary basins.
_923589
942 _cTRB
999 _c14049
_d14049