Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelso Chico. Neuquén

Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelco Chico, Neuquén. Pectolite occurs in metabasalts of the Andesitic Formation of Cerro Chapelco Chico. Neuquén. Being a hydrothermal luminiscent mineral it is a useful indicator of the presence of ore deposits...

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Detalles Bibliográficos
Autores principales:	Vattuone, M.E., Latorre, C.O., Leal, P.
Formato:	JOUR
Materias:	Chapeleó chico Mineralogy Neuquén Pectolite Zeolite/prehnite pumpellyite facies crystallography hydrothermal deposit laumontite metabasalt mineralogy Argentina
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v56_n2_p240_Vattuone
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	todo:paper_00044822_v56_n2_p240_Vattuone
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spelling	todo:paper_00044822_v56_n2_p240_Vattuone2023-10-03T13:57:37Z Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelso Chico. Neuquén Vattuone, M.E. Latorre, C.O. Leal, P. Chapeleó chico Mineralogy Neuquén Pectolite Zeolite/prehnite pumpellyite facies crystallography hydrothermal deposit laumontite metabasalt mineralogy Argentina Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelco Chico, Neuquén. Pectolite occurs in metabasalts of the Andesitic Formation of Cerro Chapelco Chico. Neuquén. Being a hydrothermal luminiscent mineral it is a useful indicator of the presence of ore deposits. It was deposited by hydrothermal fluids in veins and amygdales, in association with prehnite, laumontite, and smectite. It has a very variable habit, in most cases being found as associations of radiating blades and in globular masses, but is less commonly found as isolated idiomorphic forms of pseudotetragonal habit along the crystallographic b axis. It forms protrusions yielding a starred form, when it is known as «stellite». The crystallographic forms found are: 100. 001 and hkO. It shows simple twins with a composition plane parallel to 100 and two perpendicular cleavages 100 and 001. With a stability field ranging between 250° and 350°C at pressures below 0.3 kbar, it constitutes a good geobarometer. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v56_n2_p240_Vattuone
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Chapeleó chico Mineralogy Neuquén Pectolite Zeolite/prehnite pumpellyite facies crystallography hydrothermal deposit laumontite metabasalt mineralogy Argentina
spellingShingle	Chapeleó chico Mineralogy Neuquén Pectolite Zeolite/prehnite pumpellyite facies crystallography hydrothermal deposit laumontite metabasalt mineralogy Argentina Vattuone, M.E. Latorre, C.O. Leal, P. Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelso Chico. Neuquén
topic_facet	Chapeleó chico Mineralogy Neuquén Pectolite Zeolite/prehnite pumpellyite facies crystallography hydrothermal deposit laumontite metabasalt mineralogy Argentina
description	Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelco Chico, Neuquén. Pectolite occurs in metabasalts of the Andesitic Formation of Cerro Chapelco Chico. Neuquén. Being a hydrothermal luminiscent mineral it is a useful indicator of the presence of ore deposits. It was deposited by hydrothermal fluids in veins and amygdales, in association with prehnite, laumontite, and smectite. It has a very variable habit, in most cases being found as associations of radiating blades and in globular masses, but is less commonly found as isolated idiomorphic forms of pseudotetragonal habit along the crystallographic b axis. It forms protrusions yielding a starred form, when it is known as «stellite». The crystallographic forms found are: 100. 001 and hkO. It shows simple twins with a composition plane parallel to 100 and two perpendicular cleavages 100 and 001. With a stability field ranging between 250° and 350°C at pressures below 0.3 kbar, it constitutes a good geobarometer.
format	JOUR
author	Vattuone, M.E. Latorre, C.O. Leal, P.
author_facet	Vattuone, M.E. Latorre, C.O. Leal, P.
author_sort	Vattuone, M.E.
title	Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelso Chico. Neuquén
title_short	Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelso Chico. Neuquén
title_full	Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelso Chico. Neuquén
title_fullStr	Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelso Chico. Neuquén
title_full_unstemmed	Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelso Chico. Neuquén
title_sort	pectolite associated with laumontite and prehnite in amygdules of metabasalts. cerro chapelso chico. neuquén
url	http://hdl.handle.net/20.500.12110/paper_00044822_v56_n2_p240_Vattuone
work_keys_str_mv	AT vattuoneme pectoliteassociatedwithlaumontiteandprehniteinamygdulesofmetabasaltscerrochapelsochiconeuquen AT latorreco pectoliteassociatedwithlaumontiteandprehniteinamygdulesofmetabasaltscerrochapelsochiconeuquen AT lealp pectoliteassociatedwithlaumontiteandprehniteinamygdulesofmetabasaltscerrochapelsochiconeuquen
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Pectolite associated with laumontite and prehnite in amygdules of metabasalts. Cerro Chapelso Chico. Neuquén

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