Geology, geochemistry, and geochronology of an A‐type granite in the Mulock Glacier area, southern Victoria Land, Antarctica

@article{Cottle2006GeologyGA,
  title={Geology, geochemistry, and geochronology of an A‐type granite in the Mulock Glacier area, southern Victoria Land, Antarctica},
  author={John M. Cottle and Alan F. Cooper},
  journal={New Zealand Journal of Geology and Geophysics},
  year={2006},
  volume={49},
  pages={191 - 202}
}
  • J. Cottle, A. Cooper
  • Published 1 June 2006
  • Geology
  • New Zealand Journal of Geology and Geophysics
Abstract On the north side of the Mulock Glacier and at Cape Teall in southern Victoria Land, Antarctica, deformed greenschist facies Skelton Group metasediments are intruded by the post‐kinematic A‐type Mulock Granite. Geochemical data indicate that this intrusive complex is similar to A‐type granitoids previously described both to the north (Glee In‐trusives and Penny Hill Granite), where they form part of the Koettlitz Glacier Alkaline Province, and to the south (Foggy‐dog Granite Suite). A… 
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References

SHOWING 1-10 OF 73 REFERENCES
The Fontaine Pluton: An early Ross Orogeny calc‐alkaline gabbro from southern Victoria Land, Antarctica
Abstract The Fontaine Pluton is a previously undescribed mafic intrusion outcropping at Fontaine Bluff on the south side of the Carlyon Glacier in southern Victoria Land, Antarctica. It is the
Isotopic character of Cambro‐Ordovician plutonism, southern Victoria Land, Antarctica
Abstract Previous mapping of granitoid rocks in the Dry Valleys area of southern Victoria Land, Antarctica, identified the calc‐alkaline (DV1a), adakitic (DV1b), and monzonitic (DV2) suites. A fourth
Diorite and gabbro of the Dromedary mafic complex, South Victoria Land, Antarctica
Abstract The syntectonic Dromedary mafic complex is a well‐preserved mafic body which was emplaced into Koettlitz Group metasediments during widespread late Proterozoic‐Paleozoic granitoid plutonism,
Granitoids of the Dry Valleys area, southern Victoria Land: geochemistry and evolution along the early Paleozoic antarctic craton margin
Abstract Field relationships and geochemistry indicate granitoid plutons of the Dry Valleys area comprise at least three petrogenetically distinct suites. The older Dry Valleys 1a (DV1a) suite,
Initiation of magmatism during the Cambrian-Ordovician Ross orogeny in southern Victoria Land, Antarctica
Sensitive high-resolution ion-microprobe (SHRIMP) U-Pb zircon dating of four gneissic granitoid intrusions, whose field relationships indicate that they are among the oldest plutonic rocks exposed in
Suite subdivision and petrological evolution of granitoids from the Taylor Valley and Ferrar Glacier region, south Victoria Land
Detailed geological mapping and geochemical analysis of early Palaeozoic granitoid plutons and dykes from the Taylor Valley and Ferrar Glacier region in south Victoria Land reveal two distinct
Nature and origin of A-type granites with particular reference to southeastern Australia
In the Lachlan Fold Belt of southeastern Australia, Upper Devonian A-type granite suites were emplaced after the Lower Devonian I-type granites of the Bega Batholith. Individual plutons of two A-type
Geochemistry of the Darwin Glacier region granitoids, southern Victoria Land
The Darwin Glacier region is located between the Carlyon and Darwin glaciers in southern Victoria Land, Antarctica (Fig. 1). Previous work on Ross Orogeny granitoids of the Darwin Glacier region is
Early Cambrian carbonatite in Antarctica
Nepheline syenite bodies intrude the basement, Koettlitz Group, gneisses of the Transant-arctic Mountains of South Victoria Land, Antarctica. A calcite–fluorite–biotite–alkali feldspar dyke has
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4
5
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