Continental paleoclimates from δD and δ18O of secondary silica in paleokarst chert lags

R. Kenny, L. P. Knauth

Research output: Contribution to journalArticle

19 Citations (Scopus)

Abstract

Approximate continental palaeotemperatures can be inferred from oxygen and hydrogen isotopic analyses of authigenic silica that precipitated within chert lags on palaeokarst surfaces. Data for two Proterozoic examples suggest continental weathering temperatures that ranged from 30-43°C -from Authors

Original languageEnglish (US)
Pages (from-to)219-222
Number of pages4
JournalGeology
Volume20
Issue number3
DOIs
StatePublished - 1992

Fingerprint

paleokarst
paleotemperature
chert
paleoclimate
Proterozoic
weathering
silica
hydrogen
oxygen
temperature

ASJC Scopus subject areas

  • Geology

Cite this

Continental paleoclimates from δD and δ18O of secondary silica in paleokarst chert lags. / Kenny, R.; Knauth, L. P.

In: Geology, Vol. 20, No. 3, 1992, p. 219-222.

Research output: Contribution to journalArticle

Kenny, R. ; Knauth, L. P. / Continental paleoclimates from δD and δ18O of secondary silica in paleokarst chert lags. In: Geology. 1992 ; Vol. 20, No. 3. pp. 219-222.
@article{9b20862906a44910888ee33117977c98,
title = "Continental paleoclimates from δD and δ18O of secondary silica in paleokarst chert lags",
abstract = "Approximate continental palaeotemperatures can be inferred from oxygen and hydrogen isotopic analyses of authigenic silica that precipitated within chert lags on palaeokarst surfaces. Data for two Proterozoic examples suggest continental weathering temperatures that ranged from 30-43°C -from Authors",
author = "R. Kenny and Knauth, {L. P.}",
year = "1992",
doi = "10.1130/0091-7613(1992)020<0219:CPFDAO>2.3.CO",
language = "English (US)",
volume = "20",
pages = "219--222",
journal = "Geology",
issn = "0091-7613",
publisher = "Geological Society of America",
number = "3",

}

TY - JOUR

T1 - Continental paleoclimates from δD and δ18O of secondary silica in paleokarst chert lags

AU - Kenny, R.

AU - Knauth, L. P.

PY - 1992

Y1 - 1992

N2 - Approximate continental palaeotemperatures can be inferred from oxygen and hydrogen isotopic analyses of authigenic silica that precipitated within chert lags on palaeokarst surfaces. Data for two Proterozoic examples suggest continental weathering temperatures that ranged from 30-43°C -from Authors

AB - Approximate continental palaeotemperatures can be inferred from oxygen and hydrogen isotopic analyses of authigenic silica that precipitated within chert lags on palaeokarst surfaces. Data for two Proterozoic examples suggest continental weathering temperatures that ranged from 30-43°C -from Authors

UR - http://www.scopus.com/inward/record.url?scp=84874958671&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84874958671&partnerID=8YFLogxK

U2 - 10.1130/0091-7613(1992)020<0219:CPFDAO>2.3.CO

DO - 10.1130/0091-7613(1992)020<0219:CPFDAO>2.3.CO

M3 - Article

AN - SCOPUS:84874958671

VL - 20

SP - 219

EP - 222

JO - Geology

JF - Geology

SN - 0091-7613

IS - 3

ER -