Modal composition and detrital clinopyroxene geochemistry of lithic sandstones from the New England Fold Belt (east Australia): a Paleozoic forearc terrane.

P. A. Cawood

doi:10.1130/0016-7606(1983)94<1199:MCADCG>2.0.CO;2

Modal composition and detrital clinopyroxene geochemistry of lithic sandstones from the New England Fold Belt (east Australia): a Paleozoic forearc terrane.

P. A. Cawood

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96 Citations (Scopus)

Abstract

The Fold Belt is divided by the Peel Fault System into two time-equivalent zones showing contrasting depositional, structural, and metamorphic histories. These are inferred to represent a western magmatic arc-frontal arc succession and an eastern subduction complex assemblage. The composition of the early to middle Paleozoic clastic rocks from both east and west of the Peel Fault System indicates derivation from an undissected volcanic arc.-from Author

Original language	English
Pages (from-to)	1199-1214
Number of pages	16
Journal	GSA Bulletin
Volume	94
Issue number	10
DOIs	https://doi.org/10.1130/0016-7606(1983)94<1199:MCADCG>2.0.CO;2
Publication status	Published - 1 Jan 1983
Externally published	Yes

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Modal composition and detrital clinopyroxene geochemistry of lithic sandstones from the New England Fold Belt (east Australia): a Paleozoic forearc terrane.

Abstract

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