000			03172cam a22003618i 4500
001			22868121
003			OSt
005			20260526162636.0
008			260107t2023 njuaod frb 001 0 eng d
010			_a 2022053605
020			_a9781119417286 _q(paperback)
040			_aMdU/DLC _beng _erda _cMdU _dDLC _dclrauoh
042			_apcc
082	0	0	_a551.303
100	1		_aNichols, Gary, _eauthor.
245	1	0	_aSedimentology and stratigraphy / _cGary Nichols.
250			_aThird edition.
260			_aHoboken, NJ : _bWiley, _c2023
264		4	_c©2023
300			_axv 525 pages : _billustrations.
336			_atext _btxt _2rdacontent
337			_aunmediated _bn _2rdamedia
338			_avolume _bnc _2rdacarrier
504			_aIncludes bibliographical references and index.
505			_aSedimentary materials, processes and products -- Continental environments -- Marine environments -- Post-depsitional processes -- Stratigraphy.
520			_a"Each chapter covering environments of deposition will be divided into two sections. The first section will cover the characteristics of the modern setting, outlining the principal processes of erosion, transport and deposition. This will primarily be a geomorphological approach to sedimentology and environments. The second section will consider the products of the depositional environments in terms of what is preserved in the sedimentary record. This will be a stratigraphic approach to the products of different depositional environments. This approach is proposed to help draw a distinction between features that are important products of sedimentary processes in modern landscapes and the sedimentary products that will be preserved in the rock record. As an example, upland glacial processes create important sedimentary features in modern landscapes but are in regions of net degradation and will not be preserved in the longer-term rock record. The principle of using modern environments to interpret the sedimentary record will also be explored in more detail in terms of the limitations of the approach. Changes in the forms and diversity of plants and animals through time have very strongly impacted on sedimentary processes and products in both continental and marine environments. The differences between icehouse and greenhouse periods in Earth history also need to be taken into account when considering sedimentary environments. In particular, our current view of depositional environments is through the prism of the recent ice ages and many aspects of the greenhouse world would have looked very different. A simple uniformitarian' approach must therefore be used with care. Previous editions of the book made mention of these issues, but there will be more prominence to how changes in the planet through time impact on sedimentology"-- _cProvided by publisher.
650		0	_aSedimentation and deposition.
650		7	_alocaluoh _2Sedimentación.
650		0	_aGeology, Stratigraphic.
650		7	_aloclauoh _2Estratigrafía
856			_uhttps://itmsp.museknowledge.com/UOH?qurl=https://libros-uoh.uoh.cl//ebook_2/sedimentology-and-stratigraphy/ _yVER LIBRO DIGITAL
942			_2ddc _cBOOK _n0
999			_c6874 _d6874