ORIGIN AND GENESIS OF CALCRETE IN THE MURRAY BASIN

The Murray Basin is a shallow intracratonic sedimentary basin composed of a Cainozoic sedimentary succession that reaches a maximum thickness of 600 m in the central region (Brown & Stephenson 1991). Sedimentation was initiated with the separation of Antarctica and the southern margin of Austral...

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Bibliographic Details
Main Authors: L. N. Tylkowski, D. J. Chittleborough, K. M. Barovich
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Stephenson
Murray Basin
Antarc*
Antarctica
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.7244
http://crcleme.org.au/Pubs/Monographs/regolith2004/Tylkowski_et_al.pdf
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Summary:The Murray Basin is a shallow intracratonic sedimentary basin composed of a Cainozoic sedimentary succession that reaches a maximum thickness of 600 m in the central region (Brown & Stephenson 1991). Sedimentation was initiated with the separation of Antarctica and the southern margin of Australia (Cande & Mutter 1982) and is part of the Murray Sequence that extends from the Tertiary to the Present. Calcretes and

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