Subaerial to submarine transitions in early Miocene pyroclastic flow deposits, southern San Joaquin basin, California

R. B. Cole; P. G. Decelles

doi:10.1130/0016-7606(1991)103<0221:STSTIE>2.3.CO;2

Subaerial to submarine transitions in early Miocene pyroclastic flow deposits, southern San Joaquin basin, California

R. B. Cole, P. G. Decelles

Research output: Contribution to journal › Article › peer-review

52 Scopus citations

Abstract

The Tecuya volcanic member is an important ancient example in which the depositional environments of subaerial to submarine pyroclastic deposits are well constrained by bounding units. The characteristics of the subaerial and submarine pyroclastic flow deposits thus may be useful in other ancient volcaniclastic successions which lack bounding units of obvious paleoenvironmental origin. -from Authors

Original language	English (US)
Pages (from-to)	221-235
Number of pages	15
Journal	Geological Society of America Bulletin
Volume	103
Issue number	2
DOIs	https://doi.org/10.1130/0016-7606(1991)103<0221:STSTIE>2.3.CO;2
State	Published - 1991
Externally published	Yes

ASJC Scopus subject areas

Geology

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AB - The Tecuya volcanic member is an important ancient example in which the depositional environments of subaerial to submarine pyroclastic deposits are well constrained by bounding units. The characteristics of the subaerial and submarine pyroclastic flow deposits thus may be useful in other ancient volcaniclastic successions which lack bounding units of obvious paleoenvironmental origin. -from Authors

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Subaerial to submarine transitions in early Miocene pyroclastic flow deposits, southern San Joaquin basin, California

Abstract

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