Dextral movement on the Demon Fault, northeastern New South Wales: a reassessment ( Australia).

Citation

• McPhie, J., & Fergusson, C. L. (1983). Dextral movement on the Demon Fault, northeastern New South Wales: a reassessment ( Australia).. Journal & Proceedings - Royal Society of New South Wales, 116(3-4), 123-127.

Scopus Eid

• 2-s2.0-0020924708

Web Of Science Accession Number

Start Page

• 123

End Page

• 127

Volume

• 116

Issue

• 3-4

Place Of Publication

Abstract

• The Demon Fault is a meridional transcurrent fault extending for at least 200 km in the E part of the New England Orogen. The S margin of the Late Permian Coombadjha Volcanic Complex, and contacts between units within it, are displaced for 23 km in a dextral sense along the Fault. In the Cooraldooral Creek area the Fault consists of at least 4 major fractures. This contrasts with the Timburra River area where the trace of the Fault is marked by an elongate zone of sheared rock 500 m wide. -Authors

UOW Authors

•   Fergusson, Christopher

Publication Date

• 1983

Published In

• Journal & Proceedings - Royal Society of New South Wales  Journal

Citation

• McPhie, J., & Fergusson, C. L. (1983). Dextral movement on the Demon Fault, northeastern New South Wales: a reassessment ( Australia).. Journal & Proceedings - Royal Society of New South Wales, 116(3-4), 123-127.

Scopus Eid

• 2-s2.0-0020924708

Web Of Science Accession Number

Start Page

• 123

End Page

• 127

Volume

• 116

Issue

• 3-4

Place Of Publication