About: The influence of temperature, pH, and growth rate on the δ 18 O composition of inorganically precipitated calcite

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About: The influence of temperature, pH, and growth rate on the δ 18 O composition of inorganically precipitated calcite Goto Sponge NotDistinct Permalink

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Attributes	Values
rdf:type	Item
description	article (en) wetenschappelijk artikel (nl) наукова стаття, опублікована в жовтні 2014 (uk) im Oktober 2014 veröffentlichter wissenschaftlicher Artikel (de)
publication date	wds:Q60111412-5ACB7D3C-020A-4992-AB13-402EF4B48303
publication date	2014-10-01 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q60111412-1AE6DBCA-D58D-4707-A66E-BC3375F0E247
language of work or name	English
cites work	wds:Q60111412-EA5DE93E-807F-424B-B679-82E99F9286B4
cites work	Calibration of the calcite–water oxygen-isotope geothermometer at Devils Hole, Nevada, a natural laboratory
author name string	wds:Q60111412-0D512F4A-408E-40B5-80EF-9E86E25FAF9E wds:Q60111412-34848E2E-C87D-4F30-B570-80B41441F0FC wds:Q60111412-5D510854-6AA9-453E-9032-A8F30D14142D wds:Q60111412-BE5303F4-6C7B-4A3F-BB25-DFD4A973852C
author name string	Donald J. DePaolo James M. Watkins Frederick J. Ryerson Jonathan D. Hunt
rdfs:label	The influence of temperature, pH, and growth rate on the δ 18 O composition of inorganically precipitated calcite (en) The influence of temperature, pH, and growth rate on the δ 18 O composition of inorganically precipitated calcite (nl)
skos:prefLabel	The influence of temperature, pH, and growth rate on the δ 18 O composition of inorganically precipitated calcite (en) The influence of temperature, pH, and growth rate on the δ 18 O composition of inorganically precipitated calcite (nl)
name	The influence of temperature, pH, and growth rate on the δ 18 O composition of inorganically precipitated calcite (en) The influence of temperature, pH, and growth rate on the δ 18 O composition of inorganically precipitated calcite (nl)
title	wds:Q60111412-23B80460-F5C2-484B-B7F3-33C7E9A593BA
title	The influence of temperature, pH, and growth rate on the δ 18 O composition of inorganically precipitated calcite (en)
page(s)	wds:Q60111412-08D00753-4047-4133-A20D-E6F3017BDE87
page(s)	332-343
instance of	wds:Q60111412-84988992-B24B-4C82-8310-8009B3FEDDCE
instance of	scholarly article
main subject	wds:Q60111412-0654E1BD-34FD-4CF8-9BAE-79CE046C2E2F
main subject	geophysics
published in	wds:Q60111412-16DEC40E-E26B-44BB-89D4-E9993CC6137D
published in	Earth and Planetary Science Letters
volume	wds:Q60111412-FE4AC459-9250-42E9-AC93-5F38782A186D
volume	404
DOI	wds:Q60111412-5957BC2C-D43A-498A-A08F-EE1C43D0AF74
DOI	http://dx.doi.org/10.1016/J.EPSL.2014.07.036
DOI	10.1016/J.EPSL.2014.07.036
skos:altLabel	The influence of temperature, pH, and growth rate on the δ18O composition of inorganically precipitated calcite (en)
ADS bibcode	wds:Q60111412-6C2BC7DF-D0F4-45F1-92BE-095A264D3604
ADS bibcode	2014E&PSL.404..332W
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q60111412
is cites work of	Most Earth-surface calcites precipitate out of isotopic equilibrium Assessment of Factors Controlling Clumped Isotopes and δ18 O Values of Hydrothermal Vent Calcites The origin of carbon isotope vital effects in coccolith calcite Assessing kinetic fractionation in brachiopod calcite using clumped isotopes. Geochemistry of Vein Calcites Hosted in the Troodos Pillow Lavas and Their Implications for the Timing and Physicochemical Environment of Fracturing, Fluid Circulation, and Vein Mineral Growth Factors controlling the oxygen isotopic composition of lacustrine authigenic carbonates in Western China: implications for paleoclimate reconstructions
is cites work of	wds:Q61118478-4A8C47EF-137F-4388-8ABB-A2DE1C0B1E66 wds:Q36297934-C56D7F97-116A-4116-BDD8-84307443A766 wds:Q48262677-B553CDE1-F245-4430-B071-0DC367871492 wds:Q89702856-F95E3BA2-C27D-48EA-9F09-D69AE4BEBC40 wds:Q62638528-8A3FC0E3-5AB6-4EE7-BD89-AB1ECB4B899F wds:Q100416072-EE0D8CA4-7CEF-4DD7-A9C6-B430DD7EB909

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