K-Ar biotite ages from Miocene post-collisional Garam Chashma leucogranite, eastern Hindukush Range (Trans-Himalayas), northwestern Pakistan.
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Accession number;01A0029818
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| Title;K-Ar biotite ages from Miocene post-collisional Garam Chashma leucogranite, eastern Hindukush Range (Trans-Himalayas), northwestern Pakistan. |
| Author;
ZAFAR M
(Naruto Univ. Education, Tokushima, Jpn)
MURATA M
(Naruto Univ. Education, Tokushima, Jpn)
KHAN T
(Geological Survey Of Pakistan, Islamabad, Pak)
OZAWA H
(Naruto Univ. Education, Tokushima, Jpn)
NISHIMURA H
(Naruto Univ. Education, Tokushima, Jpn)
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Journal Title;J Mineral Petrol Sci
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Journal Code:G0150B
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ISSN:1345-6296
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VOL.95;NO.6;PAGE.101-106(2000)
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| Figure&Table&Reference;FIG.2, TBL.2, REF.27 |
| Pub. Country;Japan |
| Language;English |
| Abstract;Garam Chashma granitic rocks intrude discordantly into the Hindukush metamorphic complex on the southern margin of the Asian plate, Trans-Himalayas, northwestern Pakistan. The rocks are fine to coarse-grained, two-mica leucogranite. K-Ar biotite analyses of four samples from the Garam Chashma pluton yield 18-20 Ma ages. These ages are younger than those of the other post-collisional granitic rocks in Trans-Himalayas of Pakistan and resemble those of the Higher Himalayan granitic rocks. (author abst.) |
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