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

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

62 Scopus citations

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

Access to Document

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

Cite this

@article{93542e50fbe0459c8c4c716d97f509b0,

title = "Global distribution of Late Paleogene hiatuses.",

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)",

volume = "15",

pages = "199--203",

journal = "Geology",

issn = "0091-7613",

publisher = "Geological Society of America",

number = "3",

}

TY - JOUR

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

UR - https://www.scopus.com/pages/publications/0023140324

UR - https://www.scopus.com/pages/publications/0023140324#tab=citedBy

U2 - 10.1130/0091-7613(1987)15<199:GDOLPH>2.0.CO;2

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

M3 - Article

AN - SCOPUS:0023140324

SN - 0091-7613

VL - 15

SP - 199

EP - 203

JO - Geology

JF - Geology

IS - 3

ER -

Global distribution of Late Paleogene hiatuses.

Abstract

All Science Journal Classification (ASJC) codes

Access to Document

Other files and links

Fingerprint

Cite this