K-Ar biotite ages from Miocene post-collisional Garam Chashma leucogranite, eastern Hindukush Range (Trans-Himalayas), northwestern Pakistan.
-
- ZAFAR Mohammad
- Department of Geosciences, Faculty of Science, Naruto University of Education
-
- MURATA Mamoru
- Department of Geosciences, Faculty of Science, Naruto University of Education
-
- KHAN Tahseenullah
- Geoscience Laboratory, Geological Survey of Pakistan
-
- OZAWA Hiroaki
- Department of Geosciences, Faculty of Science, Naruto University of Education
-
- NISHIMURA Hiroshi
- Department of Geosciences, Faculty of Science, Naruto University of Education
この論文をさがす
説明
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.
収録刊行物
-
- Journal of Mineralogical and Petrological Sciences
-
Journal of Mineralogical and Petrological Sciences 95 (6), 101-106, 2000
一般社団法人 日本鉱物科学会
- Tweet
キーワード
詳細情報 詳細情報について
-
- CRID
- 1390001206544694528
-
- NII論文ID
- 10004952066
-
- NII書誌ID
- AA11460926
-
- ISSN
- 13493825
- 13456296
- http://id.crossref.org/issn/13456296
-
- 本文言語コード
- en
-
- データソース種別
-
- JaLC
- Crossref
- CiNii Articles
- OpenAIRE
-
- 抄録ライセンスフラグ
- 使用不可