Lamproite dykes in the Napier Complex at Tonagh Island, Enderby Land, East Antarctica
Lamproite dykes, discovered during JARE-40, form NS-trendmg, subvertical sheets over a 2 km distance in southeastern Tonagh Island They range from a few centimeters to one meter in thickness and up to several meters in length The lamproite is holocrystalline and consists dominantly of ferrian microc...
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Bibliographic Details
Main Authors: |
Tomoharu Miyamoto,
Edward S. Grew,
John W. Sheraton,
Martin G. Yates,
Daniel J. Dunkley,
Christopher J. Carson,
Yasutaka Yoshimura,
Yoichi Motoyoshi |
Format: | Report
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Language: | English |
Published: |
Department of Earth and Planetary Sciences, Kyushu University/Department of Geological Sciences, University of Maine/Department of Geology, Australian National University/Department of Geological Sciences, University of Maine/Gamagori Natural History Museum/Department of Geology and Geophysics, Yale University/Department of Geology, Kochi University/National Institute of Polar Research
2000
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Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3065
http://id.nii.ac.jp/1291/00003065/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3065&item_no=1&attribute_id=18&file_no=1
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