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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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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record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.578.7244 2023-05-15T13:31:07+02:00 ORIGIN AND GENESIS OF CALCRETE IN THE MURRAY BASIN L. N. Tylkowski D. J. Chittleborough K. M. Barovich The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.7244 http://crcleme.org.au/Pubs/Monographs/regolith2004/Tylkowski_et_al.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.7244 http://crcleme.org.au/Pubs/Monographs/regolith2004/Tylkowski_et_al.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://crcleme.org.au/Pubs/Monographs/regolith2004/Tylkowski_et_al.pdf text ftciteseerx 2016-01-08T12:52:54Z 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 Text Antarc* Antarctica Unknown Stephenson ENVELOPE(-69.133,-69.133,-72.133,-72.133) Murray Basin ENVELOPE(176.450,176.450,51.617,51.617)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description 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
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author L. N. Tylkowski
D. J. Chittleborough
K. M. Barovich
spellingShingle L. N. Tylkowski
D. J. Chittleborough
K. M. Barovich
ORIGIN AND GENESIS OF CALCRETE IN THE MURRAY BASIN
author_facet L. N. Tylkowski
D. J. Chittleborough
K. M. Barovich
author_sort L. N. Tylkowski
title ORIGIN AND GENESIS OF CALCRETE IN THE MURRAY BASIN
title_short ORIGIN AND GENESIS OF CALCRETE IN THE MURRAY BASIN
title_full ORIGIN AND GENESIS OF CALCRETE IN THE MURRAY BASIN
title_fullStr ORIGIN AND GENESIS OF CALCRETE IN THE MURRAY BASIN
title_full_unstemmed ORIGIN AND GENESIS OF CALCRETE IN THE MURRAY BASIN
title_sort origin and genesis of calcrete in the murray basin
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.7244
http://crcleme.org.au/Pubs/Monographs/regolith2004/Tylkowski_et_al.pdf
long_lat ENVELOPE(-69.133,-69.133,-72.133,-72.133)
ENVELOPE(176.450,176.450,51.617,51.617)
geographic Stephenson
Murray Basin
geographic_facet Stephenson
Murray Basin
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source http://crcleme.org.au/Pubs/Monographs/regolith2004/Tylkowski_et_al.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.7244
http://crcleme.org.au/Pubs/Monographs/regolith2004/Tylkowski_et_al.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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