Complejo Metamorfico de Scotia en Cabo Bowles, Isla Clarence, Shetland del Sur, Antartica.

F. Herve; R. Pankhurst; J. Davidson; C. Mpodozis

Complejo Metamorfico de Scotia en Cabo Bowles, Isla Clarence, Shetland del Sur, Antartica.

F. Herve
, R. Pankhurst
, J. Davidson
, C. Mpodozis

Engineering School

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

Abstract

Phyllite and schist samples from Cape Bowles, Clarence Island, have a greenschist-facies mineralogy. Mineralogy and total rock chemistry suggest a premetamorphic lithology of arenaceous sediments derived from an acid igneous terrain. Rb/Sr isotopic data show that metamorphism occurred during the same late Cretaceous (70-100 m.y.) event recorded elsewhere in the Scotia metamorphic complex and initial ⁸⁶Sr/⁸⁷Sr ratios are consistent with a Mesozoic rather than Precambrian source area. (Authors' abstract) -C.N.

Original language	English
Pages (from-to)	49-59
Number of pages	11
Journal	Instituto Antartico Chileno, Serie Cientifica
Volume	30
Publication status	Published - 1983

ASJC Scopus subject areas

General Environmental Science
General Earth and Planetary Sciences

Cite this

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title = "Complejo Metamorfico de Scotia en Cabo Bowles, Isla Clarence, Shetland del Sur, Antartica.",

abstract = "Phyllite and schist samples from Cape Bowles, Clarence Island, have a greenschist-facies mineralogy. Mineralogy and total rock chemistry suggest a premetamorphic lithology of arenaceous sediments derived from an acid igneous terrain. Rb/Sr isotopic data show that metamorphism occurred during the same late Cretaceous (70-100 m.y.) event recorded elsewhere in the Scotia metamorphic complex and initial 86Sr/87Sr ratios are consistent with a Mesozoic rather than Precambrian source area. (Authors' abstract) -C.N.",

author = "F. Herve and R. Pankhurst and J. Davidson and C. Mpodozis",

year = "1983",

language = "English",

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pages = "49--59",

journal = "Instituto Antartico Chileno, Serie Cientifica",

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T1 - Complejo Metamorfico de Scotia en Cabo Bowles, Isla Clarence, Shetland del Sur, Antartica.

AU - Herve, F.

AU - Pankhurst, R.

AU - Davidson, J.

AU - Mpodozis, C.

PY - 1983

Y1 - 1983

N2 - Phyllite and schist samples from Cape Bowles, Clarence Island, have a greenschist-facies mineralogy. Mineralogy and total rock chemistry suggest a premetamorphic lithology of arenaceous sediments derived from an acid igneous terrain. Rb/Sr isotopic data show that metamorphism occurred during the same late Cretaceous (70-100 m.y.) event recorded elsewhere in the Scotia metamorphic complex and initial 86Sr/87Sr ratios are consistent with a Mesozoic rather than Precambrian source area. (Authors' abstract) -C.N.

AB - Phyllite and schist samples from Cape Bowles, Clarence Island, have a greenschist-facies mineralogy. Mineralogy and total rock chemistry suggest a premetamorphic lithology of arenaceous sediments derived from an acid igneous terrain. Rb/Sr isotopic data show that metamorphism occurred during the same late Cretaceous (70-100 m.y.) event recorded elsewhere in the Scotia metamorphic complex and initial 86Sr/87Sr ratios are consistent with a Mesozoic rather than Precambrian source area. (Authors' abstract) -C.N.

UR - https://www.scopus.com/pages/publications/0020866162

M3 - Article

AN - SCOPUS:0020866162

VL - 30

SP - 49

EP - 59

JO - Instituto Antartico Chileno, Serie Cientifica

JF - Instituto Antartico Chileno, Serie Cientifica

ER -

Complejo Metamorfico de Scotia en Cabo Bowles, Isla Clarence, Shetland del Sur, Antartica.

Abstract

ASJC Scopus subject areas

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