Investigation of gold and base metals mineralization and the petrochemical studies of the associated host rocks, Shagari Bala area, Skardu GilgitBaltistan, Pakistan

Authors

  • Asad-ur-Rehman National Centre of Excellence in Geology, University of Peshawar, Pakistan
  • Mohammad Tahir Shah National Centre of Excellence in Geology, University of Peshawar, Pakistan
  • Shuhab Danishwar Khan Department of Earth and Atmospheric Sciences, University of Houston, Texas, USA
  • Laeiq Ahmad National Centre of Excellence in Geology, University of Peshawar, Pakistan

Keywords:

Gold; Base metals; Petrochemistry; Meta-volcanics; Gilgit-Baltistan

Abstract

The Shagari Bala area lies in the Skardu district of Gilgit-Baltistan province. It is located within the Kohistan-Ladakh island arc on the east side of Nanga Parbat Haramosh massif. Deosai volcanics and the meta-volcanics of the Burji-La Formation, mainly exposed in the study area are the focus of this study. The Deosai volcanics are partially to highly altered porphyrictic rocks while the meta-volcanics of the Burji-La Formation are metamorphosed to greenschist facies. The Deosai volcanics also have suldes-bearing mineralized altered zones which exhibit leaching of chalcopyrite and pyrite to malachite, azurite and limonite.

 The petrographic studies show that the Deosai volcanics have porphyritic texture and mainly comprised of plagioclase and hornblende phenocrysts. Plagioclase phenocrysts are generally partially altered but the completely altered phenocrysts are also not common. Hornblende phenocrysts are usually replaced by chlorite and epidote. Phenocrysts of plagioclase and hornblende along with alkali feldspar, quartz and ores are embedded in felsophyric groundmass. The feldspar phenocrysts and the groundmass are generally altered to kaolinite, sericite and saussurite. The meta-volcanics of the Burji-La Formation consists of amphibole (mainly tremolite/actinolite with lesser amount of hornblende), plagioclase, epidote, alkali-feldspar, chlorite and ores.  Epidote and chlorite are the alteration products of hornblende while kaolinite, sericite and saussurite are the alteration product of feldspar.

 The gain and loss in gold, silver and base metals in the hydrothermally altered suldes-bearing mineralized altered zone have been evaluated on the basis of enrichment and depletion factors. Multifold enrichment of Au, Ag and Cu are found in these zones. However, this enrichment is not of economic importance.

 The geochemical studies show that the Deosai volcanics are dacite to rhyodacite in composition while the meta-volcanics of Burji-La Formation show basalt to basaltic-andesite in composition. The spider diagrams of both Deosai volcanics and the meta-volcanics of the Burji-La Formation exhibit enrichment of large ion lithophile elements as compared to high eld strength elements while well-dened negative and positive anomalies have been observed for Nb and Sr respectively. The major and trace elements data of Deosai volanics and the meta-volcanics of the Burji-La Formation were evaluated for identifying the paleotectonic environment of their formation. It has been noticed that the studied volcanics are of calcalkaline character which have been originated in the island arc type of setting mainly involving subduction related magmatism.

References

Austromineral, 1978. Feasibility study, Mineral exploration and mining development, Development Authority, Peshawar Pakistan by Austromineral, final report, Vienna, Austria.

Bevins, R.E., Kokelaar, B.P., Dunkley, P.N., 1984. Petrology and geochemistry of lower to middle Ordovician igneous rocks in Wales: a volcanic arc to marginal basin transition. The Geologists Association Proceedings, 95, 337-347.

Danishwar, S., Stern, R.J., Khan, M.A., 2001. Field relations and structural constrains for the Teru volcanic formation, Northern Kohistan Terrane, Pakistani Himalayas. Journal of Asian Earth Sciences, 19, 683-695.

Desio, A., 1965. Sulla presenza del Cretaceo fossilifero nel vallone del Burje-la, presso Skardu (Baltistone, asia Centrale). Rendiconti della Academia nazionale dei Lincei (Rome)-Classe di scienze sche, matematiche e naturali Serie, 37, 360-364. Desio, A., 1978. On the geology of Deosai plateau (Kashmir). Memoirs Accademia Nazionale dei Lincei,15, 1-19.

Dietrich, V., Frank, W., Gansser, A., Honneger, K.H., 1983. A Jurassic–Cretaceous island arc in the Ladakh-Himalayas. Journal of Volcanology and Geothermal Research, 18, 405-433.

Frank, W., Gansser, A., Trommsdorff, V., 1977. Geological observations in the Ladakh area (Himalayas); a preliminary report. Schweizerische Mineralogische und Petro graphische Mitteilungen Bulletin, 57, 89–113.

Hamidullah, S., Jan, M.Q., Khan, B., 1992. Petrography of the Deosai volcanics, Northern Pakistan. Geological Bulletin, University of Peshawar, 25, 17-22.

Honegger, K., Dietrich, V., Frank, W., Gansser, A., Thoni, M., Trommsdortt, V., 1982. Magmatism and metamorphism in Ladakh Himalayas (the Indus Tsangpo suture zone) Earth and Planetary Science Letters, 60, 253-292.

Hubert, A.E., Chao, T.T., 1985. Determination of gold, indium, tellurium and thallium in the same sample digest of geological material by atomic absorption spectroscopy and two-step solvent extraction. Talanta, 32 (7), 568-570.

Irvine, T.N., Barager, W.R.A., 1971. A guide to the chemical clarification of the common volcanic rocks. Canadian Journal of Science, 8, 523-548.

Jeffery, P.G., Hutchison, D., 1986. Chemical Methods of Rock Analysis by Pargamon Press, Oxford.

Khan, S.D., Stern, R.J., Manton, M.I., Copeland, P., Kimura, J.I., Khan, M.A., 2004. Age geochemical and Sr-Nd-Rb isotopic constrains of mantle source characteristics and petrogenesis of Teru Volcanics, Northern Kohistan Terrane, Pakistan. Tectonophysics, 393, 263-280.

Macalalad, E., Bayoran, R., Ebarvia, B., Rubeska, I., 1988. A concise analytical scheme for 16 trace elements in geochemical exploration samples using exclusively AAS. Journal of Geochemcial Exploration, 30, 167-177.

Mullen, E.D., 1983. MnO/TiO2/P2O5: A minor element discriminant for basaltic rocks of oceanic environments and its implications for petrogenesis. Earth and Planetary Science Letters, 62, 53-62.

Pearce, J.A., Cann, J.R., 1971. Ophiolite origin investigated by discriminant analysis using Ti, Zr and Y. Earth and Planetary Science Letters, 12, 339-349.

Pearce, J.A., Cann, J.R., 1973. Tectonic setting of basic volcanic rocks determined using trace element analyses. Earth and Planetary Science Letters, 19, 290-300.

Petterson, M.G., Windley, B.F., 1991. Changing source regions of magmas and crustal growth in the Trans-Himalayas: evidence from the Chalt volcanics and Kohistan batholith, Kohistan, northern Pakistan. Earth and Planetary Science Letters, 102, 326-341.

Petterson, M.G., Windley, B.F., Luff, I.W., 1990. The Chalt volcanics, Kohistan, N. Pakistan: High-Mg tholeiitic and low-Mg calc alkaline volcanism in a Cretaceous island arc. Physics and Chemistry of the Earth, 17, 19-30.

Robertson, A.H.F., Collins, A.S., 2002. Shyok Suture Zone, N Pakistan: late Mesozoic Tertiary evolution of a critical suture separating the oceanic Ladakh Arc from the Asian continental margin. Journal of Asian Earth Science, 20, 309-351.

Rolland, Y., Pecher, A., Picard, C., 2000. Middle Cretaceous back-arc formation and arc evolution along the Asian margin: the Shyok Suture Zone in northern Ladakh (NW Himalaya). Tectonophysics, 325, 145-173.

Sharma, K.K., 1990. Petrology, geochemistry and geochronology of Ladakh batholith and its role in the evolution of Ladakh magmatic arc. Physics and Chemistry of the Earth, 17, 173-194.

Sheikh, L. Shah, M.T., Khan, S.D., 2013. Petro chemical investigation of the rocks of Golodas and surrounding areas Gilgit Baltistan, Pakistan in the perspective of gold and base metal mineralization. Unpublished MS thesis, University of Peshawar.

Sun, S.S., 1980. Lead isotopic study of young volcanic rocks from mid-ocean ridges, ocean islands and island arcs. Philosophical Transactions of the Royal Society, A297, 409-445.

Sun, S.S., McDonough, W.F., 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. In: Saunders, A.D., Norry, M.J. (Eds.), Magmatism in the Ocean Basins. Geological society of London (Special Publication) 42, 313–345.

Tahirkheli, A.K., 1974. Alluvial gold prospects in the North- West Pakistan. National Centre of Excellence in Geology, University of Peshawar, Information Release, 7. 1-50.

Vermeesch, P., 2006. Tectonic discrimination diagrams revisited. Geochemistry, Geophysics, Geosystems, 7(6), 1-68.

Wilson, M., 1989. Igneous Petrogenesis. Unwin and Hyman, London.

Wood, D.A., 1980. The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province. Earth and Planetary Science letters, 50

Downloads

Published

2015-03-31

How to Cite

Asad-ur-Rehman, Shah, M. T., Khan, S. D., & Ahmad, L. (2015). Investigation of gold and base metals mineralization and the petrochemical studies of the associated host rocks, Shagari Bala area, Skardu GilgitBaltistan, Pakistan. Journal of Himalayan Earth Sciences, 48(1), 26-40. Retrieved from http://ojs.uop.edu.pk/jhes/article/view/1958

Most read articles by the same author(s)

1 2 3 4 5 > >>