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Shallow burial dolomitization of Mid-Cenozoic, cool-water, calcitic deep-shelf limestones, southern Australia

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:5676977
 [1];  [2];  [3]
  1. Queen's Univ., Kingston, Ontario (Canada)
  2. Univ. of Adelaide (Australia)
  3. Univ. of Saskatchewan, Saskatoon (Canada)
Oligocene to middle Miocene, deep-shelf, bryozoan-rich limestones across southern Australia are variably replaced by green to orange, Ca-rich, zoned, medium-crystalline, sucrosic dolomite. The degree of replacement varies from scattered rhombs in limestone to complete dolostones a few tens of meters in thickness and a few kilometers in lateral extent. Dolostone texture ranges from dense and well lithified to completely unlithified, resembling a loose sand of dolomite rhombs. Dolomitization is fabric specific; calcite and Mg-calcite bryozoans are either the last components to be replaced or are molds. The timing and locale of dolomitization are tightly constrained; Sr isotopes indicate a middle to late Miocene age while clasts of dolostone in overlying Pliocene limestones above a regional unconformity confirm a shallow-burial, pre-Pliocene origin. {delta}{sup 13}C and {delta}{sup 18}O values support a marine source for the carbonate; the influence of meteoric fluids appears to have been negligible. Quaternary exposure has resulted in local dedolomitization and/or subaerial erosion, especially in the Murray basin. These rocks are excellent analogues for localized, lenticular dolostone bodies in calcite-rich Paleozoic platform carbonates.
OSTI ID:
5676977
Report Number(s):
CONF-910403--
Conference Information:
Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (United States) Journal Volume: 75:3
Country of Publication:
United States
Language:
English