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001 9910366643003321
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010   $a3-030-13442-3
024 7 $a10.1007/978-3-030-13442-6
035   $a(CKB)4100000007938147
035   $a(MiAaPQ)EBC5780301
035   $a(DE-He213)978-3-030-13442-6
035   $a(PPN)235670251
035   $a(EXLCZ)994100000007938147
100   $a20190411d2020      u|         0
101 0 $aeng
135   $aurcnu||||||||
181   $ctxt$2rdacontent
182   $cc$2rdamedia
183   $acr$2rdacarrier
200 10$aSediment Compaction and Applications in Petroleum Geoscience /$fby Troyee Dasgupta, Soumyajit Mukherjee
205   $a1st ed. 2020.
210  1$aCham :$cSpringer International Publishing :$cImprint: Springer,$d2020.
215   $a1 online resource (118 pages)
225 1 $aAdvances in Oil and Gas Exploration & Production,$x2509-372X
311 08$a3-030-13441-5 
327   $aPorosity development in siliclastic rocks.-Porosity development in Carbonate rocks -- Compaction Trend definition and classification -- Well logs, Seismic and Geological data in porosity and compaction trend analyses -- Deviation of normal compaction trend in relation to pore pressure -- Global examples of overpressure scenarios -- Exhumation history analysis from sonic compaction trend -- Impact of compaction trend in different tectonic- and geological setting -- Application of Porosity and compaction trend in Petroleum geoscience -- Summary.
330   $aThis book discusses how sediments compact with depth and and applications of the compaction trends. Porosity reduction in sediment conveniently indicates the degree of sediments compacted after deposition. Published empirical curves- the compaction curves- are depth-wise porosity variation through which change in pore spaces from sediment surface to deeper depths e.g. up to 6 km can be delineated. Porosity is derived from well logs. Compaction curves, referred as the Normal Porosity Profile of shales, sandstones and shale bearing sandstones of different models are reviewed along with the different mechanical and chemical compaction processes. These compaction models reveals how porosity reduces depth-wise and the probable reason for anomalous zones. Deviation from these normal compaction trends may indicate abnormal pressure scenarios: either over- or under pressure. We highlight global examples of abnormal pressure scenarios along with the different primary- and secondary mechanisms. Well logs and cores being the direct measurements of porosity, well log is the only cost-effective way to determine porosity of subsurface rocks. Certain well logs can detect overpressure and the preference of one log above the other help reduce the uncertainty. Apart from delineation of under-compacted zones by comparing the modeled- with the actual compaction, porosity data can also estimate erosion.
410  0$aAdvances in Oil and Gas Exploration & Production,$x2509-372X
606   $aSedimentology
606   $aGeology, Structural
606   $aGeology?Statistical methods
606   $aGeotechnical engineering
606   $aSedimentology$3https://scigraph.springernature.com/ontologies/product-market-codes/G17080
606   $aStructural Geology$3https://scigraph.springernature.com/ontologies/product-market-codes/G17040
606   $aQuantitative Geology$3https://scigraph.springernature.com/ontologies/product-market-codes/G17030
606   $aGeotechnical Engineering & Applied Earth Sciences$3https://scigraph.springernature.com/ontologies/product-market-codes/G37010
615  0$aSedimentology.
615  0$aGeology, Structural.
615  0$aGeology?Statistical methods.
615  0$aGeotechnical engineering.
615 14$aSedimentology.
615 24$aStructural Geology.
615 24$aQuantitative Geology.
615 24$aGeotechnical Engineering & Applied Earth Sciences.
676   $a553.28
700   $aDasgupta$b Troyee$4aut$4http://id.loc.gov/vocabulary/relators/aut$0859284
702   $aMukherjee$b Soumyajit$4aut$4http://id.loc.gov/vocabulary/relators/aut
906   $aBOOK
912   $a9910366643003321
996   $aSediment Compaction and Applications in Petroleum Geoscience$91917809
997   $aUNINA