LEADER 05448nam 2200649Ia 450 001 996210111803316 005 20230607222608.0 010 $a9786612042393 010 $a1-4443-0431-3 010 $a1-282-04239-4 010 $a1-4443-0432-1 035 $a(CKB)1000000000749593 035 $a(EBL)428299 035 $a(SSID)ssj0000306731 035 $a(PQKBManifestationID)11226556 035 $a(PQKBTitleCode)TC0000306731 035 $a(PQKBWorkID)10299164 035 $a(PQKB)11258004 035 $a(MiAaPQ)EBC428299 035 $a(OCoLC)352825770 035 $a(EXLCZ)991000000000749593 100 $a20010727d2002 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 00$aPrecambrian sedimentary environments$b[electronic resource] $ea modern approach to ancient depositional systems /$fedited by Wladyslaw Altermann & Patricia L. Corcoran 210 $aOxford, UK ;$aMalden, MA $cBlackwell Science$d2002 215 $a1 online resource (462 p.) 225 1 $aSpecial publication number 33 of the International Association of Sedimentologists 300 $aDescription based upon print version of record. 311 $a0-632-06415-3 320 $aIncludes bibliographical references and index. 327 $aIntroduction; W.ALTERMANN and P. L. CORCORAN; Introductory Papers; Actualistic versus non-actualistic conditions in the Precambrian sedimentary record: reappraisal of an enduring discussion; J. A. DONALDSON, P. G. ERIKSSON and W.ALTERMANN; The evolution of life and its impact on sedimentation; W.ALTERMANN; The significance of iron-formation in the Precambrian stratigraphic record; A. F. TRENDALL; The isotopic composition of Precambrian sulphidesaseawater chemistry and biological evolution; H. STRAUSS 327 $aDecimetre-thick encrustations of calcite and aragonite on the sea-floor and implications for Neoarchaean and Neoproterozoic ocean chemistryD. Y. SUMNER; Case Studies; The 2.7-2.63 Ga Indin Lake supracrustal belt: an Archaean marginal basin-foredeep succession preserved in the western Slave Province, Canada; S. J. PEHRSSON; Sedimentology of a tide- and wave-influenced high-energy Archaean coastline: the Jackson Lake Formation, Slave Province, Canada; W.U. MUELLER, P.L. CORCORAN and J. A. DONALDSON 327 $aThe effects of weathering, sorting and source composition in Archaean high-relief basins: examples from the Slave Province, Northwest Territories, CanadaP. L. CORCORAN and W.U.MUELLER; Stratigraphic evolution of Archaean volcanic rock-dominated rift basins from the Whim Creek Belt, west Pilbara Craton, Western Australia; G. PIKE and R. CAS; Syn- and post-eruptive volcaniclastic sedimentation in Late Archaean subaqueous depositional systems of the Black Flag Group, Eight Mile Dam, Kalgoorlie, Western Australia; J. L. HAND, R. A. F. CAS, L. ONG, S. J. A. BROWN, B. KRAPEZ and M.E. BARLEY 327 $aSedimentary environment of the amphibolite-grade Early Proterozoic Keiva and Kukas basins (north-east Baltic Shield): normative mineral MINLITH analysisO. M.ROSEN, V. T. SAFRONOV and A. A. ABBYASOV; Two meta-sedimentary basins in the Early Precambrian granulites of the Anabar Shield (polar Siberia): normative mineral compositions calculated by the MINLITH program and basin facies interpretations; V. L. ZLOBIN,O. M. ROSEN* and A. A. ABBYASOV; Mixed siliciclastic-carbonate storm-dominated ramp in a rejuvenated Palaeoproterozoic intracratonic basin: upper Hurwitz Group, Nunavut, Canada 327 $aL. B. ASPLER and J. R. CHIARENZELLIAspects of Late Palaeoproterozoic fluvial style: the Uaire?n Formation, Roraima Supergroup, Venezuela; D. G. F. LONG; Volcanogenic and sedimentary rocks within the Svecofennian Domain, Ylivieska, western Finland-an example of Palaeoproterozoic intra-arc basin fill; K. STRAND; Palaeoproterozoic epeiric sea palaeoenvironments: the Silverton Formation (Pretoria Group, Transvaal Supergroup), South Africa; P. G. ERIKSSON, W. ALTERMANN, L. EBERHARDT, S. AREND-HEIDBRINCK and A. J. BUMBY 327 $aFacies sequence and cryptic imprint of sag tectonics in the late Proterozoic Sirbu Shale, Central India 330 $aThe motivation for this volume came from the idea that the Precambrian is the key, both to the present, and to the understanding of the Earth as a whole. The Precambrian constitutes about 85% of Earth's history, and of that, about 3.75 billion years of Precambrian time, represented by rocks, are accessible to geoscientists. Ancient atmospheric and environmental conditions can be traced back to the time when the Earth was only about 250 million years old. Precambrian rocks supply almost 75% of important mineral resources such as Fe, Mn, Au, Pt and Cr. Many of these elements are associated with 410 0$aSpecial publication ... of the International Association of Sedimentologists ;$vno. 33. 606 $aGeology, Stratigraphic$yPrecambrian 606 $aSedimentation and deposition 615 0$aGeology, Stratigraphic 615 0$aSedimentation and deposition. 676 $a551.7/1 676 $a551.71 701 $aAltermann$b Wladyslaw$f1954-$0880098 701 $aCorcoran$b Patricia L$0880099 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a996210111803316 996 $aPrecambrian sedimentary environments$91965169 997 $aUNISA