Structural analysis of Bermagui area, N.S.W.
作者:
PaulF. Williams,
期刊:
Journal of the Geological Society of Australia
(Taylor Available online 1971)
卷期:
Volume 18,
issue 3
页码: 215-228
ISSN:0016-7614
年代: 1971
DOI:10.1080/00167617108728761
出版商: Taylor & Francis Group
数据来源: Taylor
摘要:
The Ordovician rocks exposed along the N.S.W. coast, near Bermagui, comprise a sequence of alternating greywacke and shale and a less abundant sequence of alternating chert and detrital beds. The only lithological boundary that can be mapped is the contact between the two sequences and it sheds little light on the large scale structure. However, due to continuity of outcrop, well‐defined vergence zones and abundant younging evidence it is possible to interpret the regional structure.
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