The geology of the Bungonia district, New South Wales.

Citation

• Carr, P. F., Jones, B. G., Kantsler, A. J., Moore, P. S., & Cook, A. C. (1980). The geology of the Bungonia district, New South Wales.. Proceedings of the Linnean Society of New South Wales, 104(3-4), 229-244.

Scopus Eid

• 2-s2.0-0019093126

Web Of Science Accession Number

Start Page

• 229

End Page

• 244

Volume

• 104

Issue

• 3-4

Abstract

• A reinterpretation of the geological history of this area in the eastern Lachlan fold belt is outlined. A Late Ordovician isoclinally folded distal flysch sequence (Tallong beds) is unconformably overlain by a Late Silurian shallow marine limestone-shale sequence (Bungonia limestone). These rocks are overlain in turn by lensoidal dacite flows interbedded with shallow marine volcaniclastic and tuffaceous sedimentary rocks (Tangerang volcanics). Emplacement of the southern part of the Marulan batholith in the Early Devonian was probably coincident with broad folding. N.C.N.S.

UOW Authors

•   Carr, Paul (external author)
•   Jones, Brian

Publication Date

• 1980

Published In

• Proceedings of the Linnean Society of New South Wales  Journal

Citation

• Carr, P. F., Jones, B. G., Kantsler, A. J., Moore, P. S., & Cook, A. C. (1980). The geology of the Bungonia district, New South Wales.. Proceedings of the Linnean Society of New South Wales, 104(3-4), 229-244.

Scopus Eid

• 2-s2.0-0019093126

Web Of Science Accession Number

Start Page

• 229

End Page

• 244

Volume

• 104

Issue

• 3-4