Hostname: page-component-cd9895bd7-jkksz Total loading time: 0 Render date: 2024-12-26T14:08:49.189Z Has data issue: false hasContentIssue false

Plagiogranites and gabbroic rocks from the Mingora ophiolitic mélange, Swat Valley, NW Frontier Province, Pakistan

Published online by Cambridge University Press:  05 July 2018

M. Barbieri
Affiliation:
Dipartimento di Scienze delia Terra, piazzale A. Moro, I-00185 Roma, Italy
A. Caggianelli
Affiliation:
DiTEc Univ. Basilicata, via N. Sauro 85, I-85100 Potenza, Italy
M. R. Di Florio
Affiliation:
Dipartimento Geomineralogico, via E. Orabona 4, I-70124 Bail, Italy
S. Lorenzoni
Affiliation:
Dipartimento Geomineralogico, via E. Orabona 4, I-70124 Bail, Italy

Abstract

Major, trace element composition and Sr isotopic data were collected for gabbroic rocks, plagiogranites and albitites in the ophiolite assemblage from Swat Valley (NW Frontier Province, Pakistan). Petrographic study revealed that these rocks were subjected to important structural and mineralogical modifications due to greenschist-epidote-amphibolite facies sub-sea-floor metamorphism and to brecciation. On the other hand, the examination of whole rock chemical composition and of chemical trends showed that these rocks were affected by some chemical modifications, concerning especially Na2O, K2O and Rb. The very low contents of HFS (high field strength) and RE elements found in gabbroic rocks and plagiogranites were considered to be a primary magmatic feature pointing in part to their cumulitic nature and in part to an origin from a refractory parental magma. The Sr isotopic data indicate that gabbroic rocks and plagiogranites were subjected to exchange with sea water. The particular chemical features shared by gabbroic rocks and plagiogranites suggested that fractional crystallization was a possible evolution process. In contrast, albitites are characterized by anomalously high contents in HFSE and LREE and by values of the 87Sr/86Sr ratio very close to sea water. These features suggest a more complex origin with respect to gabbroic rocks and plagiogranites.

Type
Petrology and Geochemistry
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1994

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Arth, J. G. (1976) Behaviour of trace elements during magmatic processes — a summary of theoretical models and their application. J. Res. U. S. Geol. Surv., 4, 41–7.Google Scholar
Boynton, W. V. (1984) Cosmochemistry of the rare earths elements: meteorite studies. In Rare Earth Element Geochemistry (P. Henderson ed.), Else-vier, 63-107.Google Scholar
Colby, J. W. (1968) Quantitative microprobe analysis of thin insulating films. Adv. X-Ray Anal., 11, 287–305.Google Scholar
Coleman, R. G. and Donato, M. M. (1979) Oceanic plagiogranite revisited. In: Trondhjemites, dacites and related rocks (F. Barker ed.), Amsterdam-Oxford-New York. Elsevier Publ. Co., 149-167.Google Scholar
Coleman, R. G. and Peterman, Z. E. (1975) Oceanic plagiogranite. J. Geophys. Res., 80, 1099–108.CrossRefGoogle Scholar
Desio, A. and Shams, F. A. (1980) The age of the blueschists and the Indus Kohistan suture line, northwest Pakistan. Ace. Naz. Lincei, 8, 74–9.Google Scholar
Dixon, S. and Rutherford, M. J. (1979) Plagiogra-nites as late-stage immiscible liquids in ophiolite and mid-ocean ridge suites: an experimental study. Earth Planet. Sci. Lett., 45, 45–60.CrossRefGoogle Scholar
Dixon Spulber, S. and Rutherford, M. J. (1983) The origin of rhyolite and plagiogranite in oceanic crust: an experimental study. J. Petrol., 24, 1–25.CrossRefGoogle Scholar
Duncan, R. A. and Green, D. H. (1987) The genesis of refractory melts in the formation of oceanic crust. Contrib. Mineral. Petrol, 96, 326–42.CrossRefGoogle Scholar
Dupuy, C, Dostal, J., Leblanc, M. (1981) Geochem-istry of an ophiolitic complex from New Caledo-nia. Contrib. Mineral. Petrol, 76, 77–83.CrossRefGoogle Scholar
Floyd, P.A. and Winchester, J.A. ( 1975) Magma type and tectonic setting discrimination using immobile elements. Earth Planet. Sci. Lett., 27, 211–8.CrossRefGoogle Scholar
Franzini, M., Leoni, L. and Saitta, M. (1972) A simple method to evaluate the Matrix Effects in X-ray fluorescence. X Ray Spectrometry, 1, 151–4.CrossRefGoogle Scholar
Franzini, M., Leoni, L. and Saitta, M. (1975) Revisione di una metodologia analitica per fluorescenza-X, basata sulla correzione completadegli effetti di matrice. Rend. Soc. Ital. Mineral. Petrol, 31, 365–78.Google Scholar
Gerlach, D. C, Leeman, W. P. and Ave Lallemant, H. G. (1981) Petrology and geochemistry of plagiogranite in the Canyon Mountain Ophio-lite, Oregon. Contrib. Mineral. Petrol., 77, 82–92.CrossRefGoogle Scholar
Hedge, C. E., Futa, K., Engel, C. G. and Fisher, R. L. (1979) Rare earth abundances and Rb-Sr systematics of basalts, gabbro, anorthosite and minor granitic rocks from Indian Ocean Ridge System, Western Indian Ocean. Contrib. Mineral. Petrol, 68, 373–6.CrossRefGoogle Scholar
Jan, Q. M., Kamal, M. and Khan, M. I. (1981) Tectonic control over emerald mineralization in Swat. Geol. Bull. Univ. Peshawar, 14, 101–9.Google Scholar
Kazmi, A. H., Lawrence, R. D., Dawood, H., Snee, L. W. and Hussain, S. S. (1984) Geology of the Indus suture zone in the Mingora-Shangla area of Swat N. Pakistan. Geol. Bull. Univ. Peshawar, 17, 127–44.Google Scholar
Kazmer, C, Hussain, S. S. and Lawrence, R. D. (1983) The Kohistan-Indian Plate suture zone at Jawan Pass, Swat, Pakistan. Geol. Soc. Amer. Ab. with Programs, 15, 609.Google Scholar
Kepezhinskas, P. and Dmitriev, D. (1992) Continental lithospheric blocks in central Atlantic Ocean. Ofioliti, 17, 19–35.Google Scholar
Leake, B. E. (1978) Nomenclature of amphiboles. Can. Mineral, 16, 501–25.Google Scholar
Lecuyer, C, Brouxel, M. and Albarede, F. (1990) Elemental fluxes hydrothermal alteration of the Trinity ophiolite (California U. S. A.) by sea-water. Chem. Geol, 89, 87–115.CrossRefGoogle Scholar
Leoni, L. and Saitta, M. (1976) Determination of Yttrium and Niobium on standard silicate rocks by X-Ray Fluorescence analysis. X-ray Spectro-metry, 5, 29–30.CrossRefGoogle Scholar
Lindsley, D. H. (1983) Pyroxene thermometry. Amer. Mineral, 68, 477–93.Google Scholar
Liou, J. G., Kuniyoshi, S. and Ito, K. (1974) Experimental studies of the phase relations between greenschist and amphibolite in a basaltic system. Amer. J. Set, 274, 613–32.Google Scholar
Liou, J. G. and Ernst, W. G. (1979) Oceanic ridge metamorphism of the east Taiwan ophiolite. Contrib. Mineral. Petrol, 68, 335–48.CrossRefGoogle Scholar
Maluski, H. and Matte, Ph. (1984) Ages of alpine tectonometamorphic events in the northwestern Himalaya (Northern Pakistan) by 39Ar/40Ar method. Tectonics, 3, 1–18.CrossRefGoogle Scholar
Moody, J. B., Meyer, D. and Jenkins, I. E. (1983) Experimental characterization of the greenschist/ amphibolite boundary in mafic system. Amer. J. Scl, 283, 48–92.CrossRefGoogle Scholar
Pearce, J.A. (1983) Role of the sub-continental lithosphere in magma genesis at active continental margins. In Continental basalts and mantle xenoliths (C.J. Hawkesworth and M.J. Norry, eds.), Shiva, Orpington (London), and Birkhauser Boston, Cambridge, Massachusetts, 230-49.Google Scholar
Pearce, J.A., Harris, N.B.W. and Tindle, A.G. (1984) Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. J. Geol, 25, 956–83.Google Scholar
Pedersen, R. B. and Malpas, J. (1984) The origin of oceanic plagiogranites from the Karmoy ophiolite, Western Norway. Contrib. Mineral. Petrol, 88, 36–52.CrossRefGoogle Scholar
Serri, G. (1981) The petrochemistry of ophiolite gabbroic complexes: a key for the classification of ophiolites into low-Ti and high-Ti types. Earth Planet. Sci. Lett., 52, 203–12.CrossRefGoogle Scholar
Sinton, J. M. and Byerly, G. R. (1980) Silicic differentiates of abyssal oceanic magmas: evidence for late-magmatic vapor transport of potassium. Earth Planet. Sci. Lett., 47, 423–30.CrossRefGoogle Scholar
Snee, L. W., Foord, E. E., Hill B. and Carter, S. J. (1989) Regional chemical differences among emeralds and host rocks of Pakistan and Afghanistan: implications for origin of emerald. In Emeralds of Pakistan. (A. H. Kazmi and L. W. Snee, eds.), Geol. Surv. of Pakistan, Quetta, 93-123.Google Scholar
Spooner, E. T. C. and Fyfe, W. S. (1973) Sub-sea-floor metamorphism, heat and mass transfer. Contrib. Mineral. Petrol, 42, 287–304.CrossRefGoogle Scholar
Tahirkheli, R. A. K. (1983) Geological evolution of Kohistan Island Arc on the Southern flank of the Karakoram-Hindu Kush in Pakistan. Boll. Geof. Teor. Appl, 25, 351–64.Google Scholar
Tahirkheli, R. A. K., Mattauer, M., Proust, F. and Tapponier, P. (1979) The India-Eurasia suture zone in the northern Pakistan: synthesis and interpretation of recent data at plate scale. In Geodynamics of Pakistan. (A. Farah and K. A. De Jong, eds.), Geol. Surv. of Pakistan, Quetta, 125-30.Google Scholar
Wildberg, H. G. H. (1987) High level and low level plagiogranites from the Nicoya ophiolite complex, Costa Rica, Central America. Geol. Rundsch., 76/1, 285–301.CrossRefGoogle Scholar