Investigation for gold and base metals mineralization and petrochemical characteristics of the rocks of Golo Das and surrounding areas, District Ghizar, Gilgit-Baltistan, Pakistan
Keywords:
Gold and base metals; Petro-chemistry; Volcanic and plutonic rocks; Golo Das; Gilgit.Abstract
Panning of stream sediments for gold along Indus River and its tributaries in the northern areas of Pakistan is being carried out for decades but the source rocks for gold are still unknown in the region. The interpretation of geochemical exploration data obtained by various geological organizations and the Remote Sensing studies conducted in the region have identified five areas for follow-up studies for gold mineralization in the Gilgit-Baltisatn region. Among these, Golo Das and surrounding areas have been investigated for gold mineralization along sulfide-bearing sheared / alteration zones during this study. The rocks exposed in the study area are highly deformed and include basalt-andesite sheet dominant volcanics and un-deformed volcanic rocks of Ishkoman Volcanic Center / Teru Volcanic Formation of Ghizar Formation and diorites of the Kohistan batholith. These rocks in Golo Das and surrounding areas are explored for their petrochemical characteristics and productive nature for gold, silver and base metals mineralization associated with sulfide-bearing sheared / alteration zones. Results of this work confirm enrichment of copper, cobalt, gold and silver in these alteration zones by hydrothermal processes but not in high concentrations to be of economic level. On the basis of major and trace element chemistry and the enrichment in large ion lithophile elements relative to high field strength element with well-defined negative Nb anomaly the rocks of the study area are comparable to the subduction related calc-alkaline rocks of island arc type setting. These rocks are, therefore, displaying subduction related signature and are considered a part of the Cretaceous Kohistan island arc.
References
Austromineral, 1976. Final report (feasibility study), Indus gold project: submitted to Pakistan Mineral Development Corporation by Austromineral, Vienna, Austria.
Austromineral, 1978. Feasibility study (final report), Mineral exploration and mining development, Chitral District: submitted to Sarhad Development Authority, Peshawar Pakistan by Austromineral, 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. Proceedings of the Geologists Association, 95, 337-347.
Danishwar, S., Stern, R.J., Khan, M.A., 2001. Field relations and structural constraints for the Teru volcanic formation, Northern Kohistan Terrane, Pakistani Himalayas. Journal of Asian Earth Sciences, 19, 683-695.
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.
Jeffery, P.G., Hutchison, D., 1986. Chemical methods of rock analysis. Pergamen 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-Pb isotopic constraints for mantle source characteristics and petrogenesis of Teru Volcanics, Northern Kohistan Terrane, Pakistan. Tectonophysics, 393, 263-280.
Khan, S.D., Walker, D.J., Hall, S., Burke, K., Shah, M.T., Stockli, L., 2009. Did KohistanLadakh island arc collide first with India? Geological Society of America Bulletin, 121 (3-4), 366-384.
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 Geochemical Exploration, 30, 167-177.
Meschede, M., 1986. A method of discriminating between different types of mid-oceanic ridge basalts and continental tholeiites with the NbZr-Y diagram. Chemical Geology, 56, 207-218.
MINORCO, 1997. Project report on re-analysis of drainage samples for northern areas of Pakistan.
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.
Petterson, M.G., Treloar, P.J., 2004. Volcanostratigraphy of arc volcanic sequences in the Kohistan arc, North Pakistan: volcanism within island arc, back-arc-basin, and intra-continental tectonic settings. Journal of Volcanology and Geothermal Research, 130, 147-178.
Petterson, M.G., Windley, B.F., 1985. Rb-Sr dating of the Kohistan arc batholith in the Himalaya of N. Pakistan. Earth and Planetary Science Letters, 74, 54-75.
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.
PMDC - Pakistan Mineral Development Corporation, 2001. Final report on geochemical exploration and evaluation of gold and base metals, northern areas, Pakistan.
Searle, M.P., Khan, M.A., 1996. Geological Map of North Pakistan and Adjacent Areas of Northern Ladakh and Western Tibet, Scale 1:650,000. Oxford University, Oxford, England.
Stolz, A.J., Jochum, K.P., Spettel, B., Hofmann, A.W., 1996. Fluid and melt related enrichment in the subarc mantle: evidence from Nb/Ta variations in island-arc basalts. Geology, 24, 587-590.
Sullivan, M.A., Windley, B.F., Saunders, A.D., Haynes, J.R., Rex, D.C., 1993. A palaeogeographic reconstruction of the Dir Group: evidence for magmatic arc migration within Kohistan, N, Pakistan. Geological Society Special Publication, 74, 139-160.
Vermeesch, P., 2006. Tectonic discrimination diagrams revisited. Geochemistry, Geophysics, Geosystems, 7(6), 1-68.
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, 11-30.