000			02890nam a22004575i 4500
001			978-3-0348-0136-2
003			DE-He213
005			20140220083253.0
007			cr nn 008mamaa
008			121227s2012 sz | s |||| 0|eng d
020			_a9783034801362 _9978-3-0348-0136-2
024	7		_a10.1007/978-3-0348-0136-2 _2doi
050		4	_aQE1-996.5
072		7	_aRBG _2bicssc
072		7	_aSCI031000 _2bisacsh
082	0	4	_a551 _223
100	1		_aGygi, Reinhart A. _eauthor.
245	1	0	_aQuantitative Geology of Late Jurassic Epicontinental Sediments in the Jura Mountains of Switzerland _h[electronic resource] / _cby Reinhart A. Gygi.
264		1	_aBasel : _bSpringer Basel : _bImprint: Birkhäuser, _c2012.
300			_aV, 216 p. 48 illus. _bonline resource.
336			_atext _btxt _2rdacontent
337			_acomputer _bc _2rdamedia
338			_aonline resource _bcr _2rdacarrier
347			_atext file _bPDF _2rda
505	0		_a1 Previous Work -- 2 What can be measured, calculated, or be quantified by comparison -- 3 Paleogeography and paleoclimate -- 4 Sedimentation -- 5 Sea level variations -- 6 Hermatypic coral assemblages: growth form, spatial distribution, and paleobathymetry -- 7 Age and time correlation of sediments -- 8 Rates of sedimentation varying between positive (net), zero, and negative (erosion) -- 9 Subsidence -- 10 Synsedimentary tectonics -- 11 Discussion and conclusions -- 12 Main conclusions -- References.
520			_aThe book summarizes about 40 years of the author’s research on sedimentary geology in an epicontinental (shelf) sea during the Late Jurassic in northern Switzerland. It presents a synopsis of the interplay of varying paleoclimate, of sea level variations, of varying water depth, of sea floor topography, of vertical and lateral facies changes, of processes of sedimentation like aggradation and progradation, of compaction, of the great regional differences in rates of sedimentation and in isostatic equilibration of the lithosphere under load, and of concomitant synsedimentary tectonics. Regional variation in isostatic adjustment of the lithosphere to the increasing load of sediments is analyzed by means of time correlations based on a detailed biochronology of ammonites in combination with mineral stratigraphy using the comparatively stable clay mineral kaolinite, and with sequence stratigraphy.
650		0	_aGeography.
650		0	_aGeology.
650		0	_aGeologyxMathematics.
650		0	_aSedimentology.
650	1	4	_aEarth Sciences.
650	2	4	_aGeology.
650	2	4	_aSedimentology.
650	2	4	_aQuantitative Geology.
710	2		_aSpringerLink (Online service)
773	0		_tSpringer eBooks
776	0	8	_iPrinted edition: _z9783034801355
856	4	0	_uhttp://dx.doi.org/10.1007/978-3-0348-0136-2
912			_aZDB-2-EES
999			_c101707 _d101707