Waiau Basin Cretaceous-Tertiary heavy minerals.

By: Smale, D.
Contributor(s): New Zealand. Dept. of Scientific and Industrial Research | New Zealand Geological Survey | New Zealand Geological Survey.
Material type: materialTypeLabelBookSeries: New Zealand Geological Survey report SL ; 12.Publisher: 1985Description: 23 p.Report number: NZGS-SL--12Subject(s): WAIAU BASIN | HEAVY MINERALS | SOUTHLAND | CRETACEOUS | TERTIARY | SEDIMENTS | TAKATIMU | LONGWOOD | FIORDLAND | NZMS260C45 | NZMS260C46 | NZMS260D45 | NZMS260D46 | PROVENANCE | WAIAU RIVER (SOUTHLAND) | TUATAPERE | ORAUEA | LILLBURN | RATABURN | WAITUTU RIVER | LAKE POTERITERI | LAKE HAUROKO | WAIRAURAHIRI RIVER | WAITAPU | NZMS262 16
Incomplete contents:
Heavy minerals from Tertiary sediments in the Waiau Basin suggest that most of the western sediments were derived locally from adjacent basement rocks of the Fiordland Complex. A greater proportion of semi- opaque debris in the eastern sediments suggests derivation from the Takitimu Mountains or Longwood Range. Ilmenite, magnetite, biotite, sphene, epidote, and hornblende are widespread in the sediments and in the basement rocks, though hornblende and biotite tend to fluctuate sidely. Only the Sand Hill Point Formation, while still being dominantly Fiordland-derived, was not derived from the immediately adjacent basement. The distinctive minerals aegerine-augite and riebeckite occur only near the upper Lill Burn. Impoverishment of apatite in the eastern part of the basin is probably due to solution through acid weathering. Factor analysis suggests that in two major sampled area (Lill Burn and Track Burn) an epidote-sphene assemblage contributed sediment to coal measures. In approximately Whaingaroan times the epidote-sphene assemblage was replaced by an impoverished ilmenite-zircon assemblage. Because this is the reverse of the situation in coal measures studied elsewhere in Southland and in Canterbury, the ilmenite-zircon assemblage was probably inherited from the provenance area rather than the result of intrastratal solution
Tags from this library: No tags from this library for this title. Log in to add tags.
Item type Current location Call number Copy number Status Date due Barcode
ABSTRACT ABSTRACT NIWA BIBLIOGRAPHY
1 Available 51185-1001

14 refs; 1 fig; 4 tables

Heavy minerals from Tertiary sediments in the Waiau Basin suggest that most of the western sediments were derived locally from adjacent basement rocks of the Fiordland Complex. A greater proportion of semi- opaque debris in the eastern sediments suggests derivation from the Takitimu Mountains or Longwood Range. Ilmenite, magnetite, biotite, sphene, epidote, and hornblende are widespread in the sediments and in the basement rocks, though hornblende and biotite tend to fluctuate sidely. Only the Sand Hill Point Formation, while still being dominantly Fiordland-derived, was not derived from the immediately adjacent basement. The distinctive minerals aegerine-augite and riebeckite occur only near the upper Lill Burn. Impoverishment of apatite in the eastern part of the basin is probably due to solution through acid weathering. Factor analysis suggests that in two major sampled area (Lill Burn and Track Burn) an epidote-sphene assemblage contributed sediment to coal measures. In approximately Whaingaroan times the epidote-sphene assemblage was replaced by an impoverished ilmenite-zircon assemblage. Because this is the reverse of the situation in coal measures studied elsewhere in Southland and in Canterbury, the ilmenite-zircon assemblage was probably inherited from the provenance area rather than the result of intrastratal solution

GS

There are no comments on this title.

to post a comment.

Powered by Koha