A Paleomagnetic Reconnaissance of some late Precambrian to Early Paleozoic Rocks of Tansen Area, Lesser Himalaya, Nepal
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説明
For a preliminary paleomagnetic research on Late Precambrian to Early Paleozoic rocks in the Tansen area (West Central Nepal) carbonate, sandstone, quartzite and slate were collected from 30 sites at 4 localities. Detailed analyses of magnetic remanence were made using alternating field and thermal demagnetization techniques. Most of the specimens were found to be weakly magnetized (intensities of 10^-7 emu/cc, in order). Three magnetic components have been distinguished: (1) a predominant secondary component of recent origin, which represents a larger portion of the magnetization intensity in weakly magnetized specimens and thus hinders the separation of primary components. (2) another component (probably secondary), which yields a mean direction: D=320°, I=10°, a95=21° (before bedding correction) restricted only to purple slate varieties of Ramdighat Formation, and (3) a probably characteristic mean direction: D=350°, I=-45°, a95=15° derived from carbonate rock specimens of Kerabari Formation. This direction gives a virtual geomagnetic south pole position at 36°S/95°E.
収録刊行物
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- 北海道大学理学部紀要
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北海道大学理学部紀要 22 (2), 259-275, 1987-08
北海道大学
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詳細情報 詳細情報について
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- CRID
- 1050282813974253568
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- NII論文ID
- 120001152055
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- HANDLE
- 2115/36749
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- ISSN
- 00183474
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- 本文言語コード
- en
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- 資料種別
- departmental bulletin paper
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- データソース種別
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- IRDB
- CiNii Articles