Post-Early Cretaceous landform evolution along the western margin of the Bancannia Trough, western NSW  


Authors / CoAuthors

Gibson, D.L.

Abstract

Previously undated post Devonian sediments are shown by plant macro- and microfossils to be Early Cretaceous, and thus part of the Eromanga Basin. Modern landscape in the northern Barrier Ranges results from differential erosion following post-Early Cretaceous deformation that folded these and underlying rocks, most probably in response to reverse movements on faults at the western margin of the Bancannia Trough.

Product Type

nonGeographicDataset

eCat Id

38514

Contact for the resource

  Custodian

 

  Point of contact

Commonwealth of Australia (Geoscience Australia)  
Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
ACT
2601
Australia

Keywords

  • External PublicationScientific Journal Paper
( Theme )
  • landforms
( Theme )
  • palaeogeography
( Theme )
  • palaeontology
( Theme )
  • structural geology
( Theme )
  • stratigraphy
  • AU-NSW
Australian and New Zealand Standard Research Classification (ANZSRC)
  • Earth Sciences
  • Published_Internal

Publication Date

2000-01-01T00:00:00

Creation Date

Security Constraints

Australian Government Security ClassificationSystem    

Classification - unclassified

Legal Constraints

Creative Commons Attribution 4.0 International Licence    

Access - restricted

Use - license

Status

Purpose

Maintenance Information

unknown

Topic Category

geoscientificInformation

Series Information

22(1)

Lineage

Unknown

Parent Information

Extents

[-31.08, -30.45, 141.58, 141.92]

Reference System

Spatial Resolution

Service Information

Associations

Downloads and Links

Source Information

Source data not available.