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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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 |