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001436014 001__ 1436014
001436014 003__ OCoLC
001436014 005__ 20230309004004.0
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001436014 019__ $$a1248685493
001436014 020__ $$a9783030639822$$q(electronic bk.)
001436014 020__ $$a3030639827$$q(electronic bk.)
001436014 020__ $$z9783030639815
001436014 020__ $$z3030639819
001436014 0247_ $$a10.1007/978-3-030-63982-2$$2doi
001436014 035__ $$aSP(OCoLC)1247828703
001436014 040__ $$aYDX$$beng$$erda$$epn$$cYDX$$dGW5XE$$dOCLCO$$dEBLCP$$dOCLCF$$dUKAHL$$dOCLCQ$$dCOM$$dOCLCO$$dOCLCQ
001436014 043__ $$au-at---
001436014 049__ $$aISEA
001436014 050_4 $$aQE471.15.C3
001436014 08204 $$a552/.5099423$$223
001436014 1001_ $$aJames, Noel P.,$$eauthor.
001436014 24510 $$aBiogenic sedimentary rocks in a cold, Cenozoic ocean :$$bneritic Southern Australia /$$cNoel P. James, Yvonne Bone.
001436014 264_1 $$aCham :$$bSpringer,$$c[2021]
001436014 300__ $$a1 online resource :$$billustrations
001436014 336__ $$atext$$btxt$$2rdacontent
001436014 337__ $$acomputer$$bc$$2rdamedia
001436014 338__ $$aonline resource$$bcr$$2rdacarrier
001436014 504__ $$aIncludes bibliographical references and index.
001436014 5050_ $$a1. Setting -- 2. Modern Sedimentology -- 3. Cenozoic Depositional Basins -- 4. Geohistory and Sedimentary Successions -- 5. SA2 Eocene Early Oligocene -- 6. SA3 Upper Ologocene-Mid Miocene -- 7. SA4 Plio-Pleistocene -- 8. Pre-Uplift -- 9. Post Uplift.
001436014 506__ $$aAccess limited to authorized users.
001436014 520__ $$aThis book documents and interprets the onshore Cenozoic temperate carbonate depositional system along the southern margin of Australia. These strata, deposited in four separate basins, together with the extensive modern marine system offshore, comprise the largest such cool-water carbonate system on the globe. The approach is classic and comparative but the information is a synthesis of recent research and new information. A brief section of introduction outlines the setting, modern comparative sedimentology offshore, and structure of the Cenozoic onshore. The core of the book is a detailed analysis and illustration of the four Eocene to Pleistocene successions. Deposits range from temperate carbonates, to biosiliceous spiculites, to marginal marine siliciclastics. Each unit is interpreted, as much as possible, based on our understanding of the modern offshore depositional system. A subsequent part concentrates on diagenesis both before and after the late Miocene uplift. It turns out that alteration in the two packages is entirely different. The preceding attributes of each succession are then interpreted on the basis of controlling factors such as tectonics, oceanography, climate, and glaciation of nearby Antarctica. This research has revealed new implications for the interpretation of specific attributes of cool-water carbonate sedimentology that could only be discovered from the rock record. Insights concerning cyclicity, reef mounds, biosiliceous deposition, and trophic resources are detailed in the next section. The concluding part focuses on global comparisons, especially the Mediterranean and New Zealand.
001436014 588__ $$aOnline resource; title from PDF title page (SpringerLink, viewed April 27, 2021).
001436014 650_0 $$aCarbonate rocks$$zAustralia$$zSouth Coast.
001436014 650_0 $$aGeology, Stratigraphic$$yCenozoic.
001436014 650_0 $$aSedimentology$$zAustralia$$zSouth Coast.
001436014 650_6 $$aStratigraphie$$yCénozoïque.
001436014 655_0 $$aElectronic books.
001436014 7001_ $$aBone, Yvonne,$$eauthor.
001436014 77608 $$iPrint version:$$aJames, Noel P.$$tBiogenic sedimentary rocks in a cold, Cenozoic ocean.$$dCham : Springer, [2021]$$z3030639819$$z9783030639815$$w(OCoLC)1201380843
001436014 852__ $$bebk
001436014 85640 $$3Springer Nature$$uhttps://univsouthin.idm.oclc.org/login?url=https://link.springer.com/10.1007/978-3-030-63982-2$$zOnline Access$$91397441.1
001436014 909CO $$ooai:library.usi.edu:1436014$$pGLOBAL_SET
001436014 980__ $$aBIB
001436014 980__ $$aEBOOK
001436014 982__ $$aEbook
001436014 983__ $$aOnline
001436014 994__ $$a92$$bISE