Printer Friendly

U-Pd zircon ages for the Chinglai gneiss, lower Buner, North Pakistan.

Byline: Irshad Ahmad, Shuhab, D. Khan and Tom Lappen

The Chinglai gneiss is a dark-colored medium-grained rock characterized by abundant augen of k-feldspar and plagioclase. It is located on the western limb of the Indus syntaxis. The Chinglai gneiss was initially mapped as part of the Ambela complex (Siddiqui et al., 1968; Rafiq, 1987). The Ambela complex was considered to be late Paleozoic on the basis of whole-rock Rb-Sr (297 + 4, 315 + 15) and U-Pb zircon (280 + 15) ages from the Koga syenite (Le Bas et al., 1987 and Smith et al., 1994 respectively) and the intrusive contact of the Ambela granites with Carboniferous rock of the Jaffar Kandao Formation, where the Chinglai gneiss was also considered Carboniferous in age. Sak and Pogue (1995) and Khan et al. (1990) mapped the Chinglai gneiss as a separate body and is in contact with Ambela granite and the Ambar Formation.

They considered the Chinglai gneiss to be of Cambrian age. DiPietro et al. (1999) based on texture and composition similar to Swat gneisses mapped the Chinglai gneiss and the southeastern part of the Ambela complex as part of the Swat gneisses. The Swat gneisses were previously correlated with the Mansehra gneiss that is considered to be late Cambrian on the basis of a whole-rock Rb-Sr age of 516 + 16 Ma (Le Fort et al., 1980). Anckeiwicz (1998) obtained U-Pb zircon age of 468 + 5 Ma from the Choga granodiorite gneiss and ca. 265 Ma from Ilam body part of the Swat gneiss to be related with late Paleozoic event.

Chinglai gneiss has abundant zircon. A sample from the Chinglai gneiss along the main road from Chinglai-Totalai section was collected for zircon separation. Zircons were separated using standard techniques of crushing, grinding and heavy liquid and magnetic separation. Zircons picked were clear euhedral grains of two morphologies, elongated prisms or stuby prisms. Analyses were performed at the Department of Earth and Atmospheric Sciences, University of Houston, using Laser ablation ICP-MS. Cathodoluminesnce (CL) images of the zircon show zoning and inherited cores (Fig. 1). In total of 17 analyses were carried out on multi grains.

The analyses obtained show an upper intercept 827 Ma from the inherited core. This age is in agreement with the Black mountain complex of 823 Ma age (U-Pb zircon, DiPietro and Iscachsen, 2001) in the east of the Chinglai gneiss. The lower intercept of 456 represents a younger Pb loss and/or overgrowth associated with the intrusion in the north, the Choga granodiorite gneiss having U-Pb zircon age of 468 + 5 (Anckiewicz et al., 1998).

The present age of 826 Ma from the inherited core and 456 Ma from the rim for the Chinglai gneiss supports the above interpretation. It constrained the age of the Gandaf and the Tanwal Formations regarded as Proterozoic and Cambrian respectively (Sak and Pogue, 1995). This also supports the argument that the Chinglai gneiss is not genetically related to the Ambela granitic complex (Khan et al., 1990; DiPietro et al., 1999).

DiPietro and Iscachsen (2001) regarded the 823 Ma age for the Black Mountain as minor Late Proterozoic intrusive event and possibly correlative with Malani magmatism which has been dated between 750 and 850 Ma on the Aravalli craton of northern India and with a ca. 870 Ma igneous suite from the Kirana Hills in Pakistan (Kazmi and Jan, 1997).

References

Anczkiewicsz., R., Oberli, F., Burg, J.P., Meier, M. Dawood, H. and Hussain, S. S., 1998. Magmatism south of the Indus suture, lower Swat, Pakistan. Geological Bulletin, University of Peshawar, Special issue, 31, 7-9.

DiPietro, J.A., Pogue, K.P., Hussain, A. and Ahmad, I., 1999. Geological map of the Indus Syntaxis and surrounding area, northwest Himalaya, Pakistan. Geological Society of America Special Paper 328, 159-178.

DiPietro, J. A., Isachsen, C. E., 2001. U-Pb zircon ages from the Indian plate in northwest Pakistan and their significance to Himalayan and pre-Himalayan geologic history. Tectonics 20, 510-525.

Kazmi, A.H., Jan, M.Q., 1997. Geology and Tectonics of Pakistan. Graphic Publishers, Karachi Pakistan.

Khan, S.R., Khan, M.A., Nawaz R., Karim, T. 1990. Stratigraphic control for the age of Peshawar plain magmatism, north Pakistan. Geological Bulletin, University of Peshawar, 23, 253-263.

Le Bas, M.J., Mian, I., Rex, D.C., 1987. Age and nature of carbonatite emplacement in north Pakistan: Geol. Rundschau, 76(2), 317-323.

Le Fort, P., Debon, F., Sonet, J., 1980. The "Lesser Himalayan" cordierite granite belt, typology and age of the pluton of Manserah, Pakistan. Geological Bulletin, University of Peshawar, 13, 51-62.

Rafiq, M., 1987. Petrology and geochemistry of Ambela garnitic complex, N.W.F.P. Pakistan. Unpublished Ph.D. thesis, University of Peshawar.

Siddiqui, S.F.A., Chaudhry, M.N., Shakoor, A., 1968. Geology and petrology of felspathoidal syenites and associated rocks of Koga area, Chamla valley, Swat, West Pakistan. Geological Bulletin, Punjab University, 7, 1-30.

Sak, P.B., Pogue, K.R., 1995. Petrographic and microstructural analysis of granitic rocks from the Indus syntaxis region, northern Pakistan. Geological Society of America Abstracts with Programs, 27(6), p. 391.

Smith, H.A., Chamberlain, C.P., Zietler, P.K., 1994. Timing and duration of Himalaya metamorphism within the Indian plate, northwest Himalaya, Pakistan. Journal of Geology, 102, 493-503.

Irshad Ahmad, NCE in Geology, University of Peshawar, Peshawar.

Shuhab, D. Khan Department of Earth and Atmospheric Sciences, University of Houston, TX 77204, USA and

Tom Lappen, Department of Earth and Atmospheric Sciences, University of Houston, TX 77204, USA.
COPYRIGHT 2010 Asianet-Pakistan
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 2010 Gale, Cengage Learning. All rights reserved.

Article Details
Printer friendly Cite/link Email Feedback
Author:Ahmad, Irshad; Shuhab, D. Khan; Lappen, Tom
Publication:Journal of Himalayan Earth Sciences
Article Type:Report
Geographic Code:9PAKI
Date:Dec 31, 2010
Words:905
Previous Article:Numerical modeling of conjugate 'Riedel' deformation bands in sandstone.
Next Article:Site amplification factor at Mardan, Pakistan.
Topics:

Terms of use | Privacy policy | Copyright © 2019 Farlex, Inc. | Feedback | For webmasters