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Biogenic sedimentary rocks in a cold...

Bone, Yvonne.

Biogenic sedimentary rocks in a cold, Cenozoic oceanneritic Southern Australia /

Record Type:	Electronic resources : Monograph/item
Title/Author:	Biogenic sedimentary rocks in a cold, Cenozoic oceanby Noel P. James, Yvonne Bone.
Reminder of title:	neritic Southern Australia /
Author:	James, Noel P.
other author:	Bone, Yvonne.
Published:	Cham :Springer International Publishing :2021.
Description:	xxxii, 217 p. :ill., digital ;24 cm.
Contained By:	Springer Nature eBook
Subject:	Carbonate rocksAustralia
Online resource:	https://doi.org/10.1007/978-3-030-63982-2
ISBN:	9783030639822$q(electronic bk.)

Biogenic sedimentary rocks in a cold, Cenozoic oceanneritic Southern Australia /
James, Noel P.

Biogenic sedimentary rocks in a cold, Cenozoic oceanneritic Southern Australia /[electronic resource] :by Noel P. James, Yvonne Bone. - Cham :Springer International Publishing :2021. - xxxii, 217 p. :ill., digital ;24 cm.

1. 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.

This 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.

ISBN: 9783030639822$q(electronic bk.)

Standard No.: 10.1007/978-3-030-63982-2doiSubjects--Topical Terms:

890996
Carbonate rocks
--Australia

LC Class. No.: QE471.15.C3 / J364 2021

Dewey Class. No.: 552.5099423

Biogenic sedimentary rocks in a cold, Cenozoic oceanneritic Southern Australia /
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505 0 $a 1. 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.
520 $a This 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.
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