PREHNITE.PUMPELLYITE FACIES METAMORPHISM OF THE NEW BAY FORIVIATION, EXPLO|TS ZONE, NEWFOUNDLAND

wedge of andesitic volcaniclastic sediments inter-preted to have been deposited in an early Paleozoic arc-trench gap. The sediments have been meta' morphosed to prehnite-pumpellyite facies, but pum-pellyite is not common. A characteristic mineral assemblage is albite-f calcite + quartz f prehni...

Full description

Bibliographic Details
Main Author: Stephen G. Franks
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Newfoundland
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.528.5099
http://rruff.info/doclib/cm/vol12/CM12_456.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.528.5099
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.528.5099 2023-05-15T17:21:47+02:00 PREHNITE.PUMPELLYITE FACIES METAMORPHISM OF THE NEW BAY FORIVIATION, EXPLO|TS ZONE, NEWFOUNDLAND Stephen G. Franks The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.528.5099 http://rruff.info/doclib/cm/vol12/CM12_456.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.528.5099 http://rruff.info/doclib/cm/vol12/CM12_456.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://rruff.info/doclib/cm/vol12/CM12_456.pdf text ftciteseerx 2016-01-08T10:27:47Z wedge of andesitic volcaniclastic sediments inter-preted to have been deposited in an early Paleozoic arc-trench gap. The sediments have been meta' morphosed to prehnite-pumpellyite facies, but pum-pellyite is not common. A characteristic mineral assemblage is albite-f calcite + quartz f prehnite * chlorite 4 epidote. Field relations and mineral assemblages are interpreted as intlicating metamor-phism at temperatures on the order of 300*400'C and load pressures less than 1 kb. The high temper' atures were produced by injection of numerous thick dykes and sills which were feeders to the over-lying Lawrence Head pillow lavas. Text Newfoundland Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description wedge of andesitic volcaniclastic sediments inter-preted to have been deposited in an early Paleozoic arc-trench gap. The sediments have been meta' morphosed to prehnite-pumpellyite facies, but pum-pellyite is not common. A characteristic mineral assemblage is albite-f calcite + quartz f prehnite * chlorite 4 epidote. Field relations and mineral assemblages are interpreted as intlicating metamor-phism at temperatures on the order of 300*400'C and load pressures less than 1 kb. The high temper' atures were produced by injection of numerous thick dykes and sills which were feeders to the over-lying Lawrence Head pillow lavas.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Stephen G. Franks
spellingShingle Stephen G. Franks
PREHNITE.PUMPELLYITE FACIES METAMORPHISM OF THE NEW BAY FORIVIATION, EXPLO|TS ZONE, NEWFOUNDLAND
author_facet Stephen G. Franks
author_sort Stephen G. Franks
title PREHNITE.PUMPELLYITE FACIES METAMORPHISM OF THE NEW BAY FORIVIATION, EXPLO|TS ZONE, NEWFOUNDLAND
title_short PREHNITE.PUMPELLYITE FACIES METAMORPHISM OF THE NEW BAY FORIVIATION, EXPLO|TS ZONE, NEWFOUNDLAND
title_full PREHNITE.PUMPELLYITE FACIES METAMORPHISM OF THE NEW BAY FORIVIATION, EXPLO|TS ZONE, NEWFOUNDLAND
title_fullStr PREHNITE.PUMPELLYITE FACIES METAMORPHISM OF THE NEW BAY FORIVIATION, EXPLO|TS ZONE, NEWFOUNDLAND
title_full_unstemmed PREHNITE.PUMPELLYITE FACIES METAMORPHISM OF THE NEW BAY FORIVIATION, EXPLO|TS ZONE, NEWFOUNDLAND
title_sort prehnite.pumpellyite facies metamorphism of the new bay foriviation, explo|ts zone, newfoundland
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.528.5099
http://rruff.info/doclib/cm/vol12/CM12_456.pdf
genre Newfoundland
genre_facet Newfoundland
op_source http://rruff.info/doclib/cm/vol12/CM12_456.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.528.5099
http://rruff.info/doclib/cm/vol12/CM12_456.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766107435671486464

Similar Items