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Pre-obduction records of Eocene foreland basins in central New Caledonia: an appraisal from surface geology and Cadart-1 borehole data.
- Source :
- New Zealand Journal of Geology & Geophysics; Sep2014, Vol. 57 Issue 3, p300-311, 12p
- Publication Year :
- 2014
-
Abstract
- The Bourail Anticline in central New Caledonia has been a target for petroleum exploration since the 1950s. It is a broad structure in which a 4-km-thick pile of Eocene turbidite (Eocene Bourail Flysch) is exposed. The Cadart-1 exploration borehole (1930 m deep) was drilled on the anticlinal axis in 1999, intersecting the Paleogene and underlying Late Cretaceous sedimentary rocks. A sedimentological, stratigraphic and provenance analysis is presented. Volcanic debris appears progressively in the upper part of the flysch, becoming predominant upwards along with the intercalation of upward-thickening and -coarsening debris flow breccia. Clinopyroxene and basalt clasts in the upper part of the flysch were derived from enriched tholeiite (E-MORB) of the Poya Terrane. The Eocene paleogeography can be interpreted as a foreland basin system with a depocentre close to the area of Bourail Anticline, an accretionary complex to the northwest and a forebulge to the southeast. This system migrated southeastward through New Caledonia from the Paleocene to the Late Eocene. [ABSTRACT FROM AUTHOR]
- Subjects :
- GEOLOGICAL basins
EOCENE Epoch
TURBIDITES
FLYSCH
FACIES
SEDIMENTARY rocks
Subjects
Details
- Language :
- English
- ISSN :
- 00288306
- Volume :
- 57
- Issue :
- 3
- Database :
- Complementary Index
- Journal :
- New Zealand Journal of Geology & Geophysics
- Publication Type :
- Academic Journal
- Accession number :
- 98053339
- Full Text :
- https://doi.org/10.1080/00288306.2014.885065