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={J. Cottle and A. Cooper},
  journal={New Zealand Journal of Geology and Geophysics},
  year={2006},
  volume={49},
  pages={191 - 202}
}
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… Expand
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