Global distribution of Late Paleogene hiatuses.

Gerta Keller; T. Herbert; R. Dorsey; S. D'Hondt; M. Johnsson; W. R. Chi

doi:10.1130/0091-7613(1987)15<199:GDOLPH>2.0.CO;2

Global distribution of Late Paleogene hiatuses.

Gerta Keller, T. Herbert, R. Dorsey, S. D'Hondt, M. Johnsson, W. R. Chi

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Abstract

Six global late Paleogene hiatuses (PHa to PHe) have been identified from deep-sea sequences. These hiatuses occurred at the middle/late Eocene boundary, late Eocene, Eocene/Oligocene boundary, late early Oligocene, late Oligocene, and Oligocene/Miocene boundary horizons. These hiatuses may have been caused by basin-shelf fractionation of carbonates.-from Authors

Original language	English (US)
Pages (from-to)	199-203
Number of pages	5
Journal	Geology
Volume	15
Issue number	3
DOIs	https://doi.org/10.1130/0091-7613(1987)15<199:GDOLPH>2.0.CO;2
State	Published - 1987

All Science Journal Classification (ASJC) codes

Geology

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10.1130/0091-7613(1987)15<199:GDOLPH>2.0.CO;2

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abstract = "Six global late Paleogene hiatuses (PHa to PHe) have been identified from deep-sea sequences. These hiatuses occurred at the middle/late Eocene boundary, late Eocene, Eocene/Oligocene boundary, late early Oligocene, late Oligocene, and Oligocene/Miocene boundary horizons. These hiatuses may have been caused by basin-shelf fractionation of carbonates.-from Authors",

author = "Gerta Keller and T. Herbert and R. Dorsey and S. D'Hondt and M. Johnsson and Chi, {W. R.}",

year = "1987",

doi = "10.1130/0091-7613(1987)15<199:GDOLPH>2.0.CO;2",

language = "English (US)",

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T1 - Global distribution of Late Paleogene hiatuses.

AU - Keller, Gerta

AU - Herbert, T.

AU - Dorsey, R.

AU - D'Hondt, S.

AU - Johnsson, M.

AU - Chi, W. R.

PY - 1987

Y1 - 1987

N2 - Six global late Paleogene hiatuses (PHa to PHe) have been identified from deep-sea sequences. These hiatuses occurred at the middle/late Eocene boundary, late Eocene, Eocene/Oligocene boundary, late early Oligocene, late Oligocene, and Oligocene/Miocene boundary horizons. These hiatuses may have been caused by basin-shelf fractionation of carbonates.-from Authors

AB - Six global late Paleogene hiatuses (PHa to PHe) have been identified from deep-sea sequences. These hiatuses occurred at the middle/late Eocene boundary, late Eocene, Eocene/Oligocene boundary, late early Oligocene, late Oligocene, and Oligocene/Miocene boundary horizons. These hiatuses may have been caused by basin-shelf fractionation of carbonates.-from Authors

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JO - Geology

JF - Geology

IS - 3

ER -

Global distribution of Late Paleogene hiatuses.

Abstract

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