Crystallization conditions and petrogenesis of the paleoproterozoic basement rocks in Bangladesh: An evaluation of biotite and coexisting amphibole mineral chemistry
Tóm tắt
The Paleoproterozoic (∼1.73 Ga) basement rocks from Maddhapara, Bangladesh show a large range of chemical variations including diorite, quartz diorite, monzodiorite, quartz monzonite and granite. These are composed of varying proportions of quartz+plagioclase+K-feldspar+biotite+ hornblende±epidote+titanite+magnetite+apatite and zircon. Amphibole and biotite, dominant ferromagnesian minerals, have been analyzed with an electron microprobe. The biotite, Mg-dominant trioctahedral micas, is classified as phlogopitic nature. Relatively high Mg (1.33–1.53 pfu), Mg# (0.52–0.59) and low AlVI (0.13–0.25 pfu) contents in the biotite reflect slightly fractionated magma, which might be a relative indicator for the origin of the parental magma. Biotite is also a very good sensor of oxidation state of the parental magma. Oxygen fugacity of the studied biotites estimate within the QFM and HM buffers and equilibrate at about −12.35 and −12.46, which exhibit the source materials were relatively higher oxidation state during crystallization and related to arc magmatism. Whereas, calcic amphiboles, a parental member of arc-related igneous suite, display consistent oxygen fugacity values (−11.7 to −12.3), low Al# (0.16–0.21) with H2Omelt (5.6 wt.%–9.5 wt.%) suggest their reliability with the typical values of calc-alkaline magma crystallization. The oxygen fugacity of magma is related to its source material, which in turn depends on tectonic setting. Discrimination diagrams and chemical indices of both biotite and amphibole of dioritic rocks reveal calc-alkaline orogenic complexes; mostly I-type suite formed within subduction-related environments. Moreover, igneous micas are used as metallogenic indicator. The biotites with coexisting amphibole compositions show an apparent calc-alkaline trend of differentiation. The study suggests that the trend of oxidized magmas is commonly associated with compressive tectonic and convergent plate boundaries.
Tài liệu tham khảo
Abdel-Rahman, A. F. M., 1994. Nature of Biotites from Alkaline, Calc-Alkaline, and Peraluminous Magmas. Journal of Petrology, 35(2): 525–541
Allen, J. C., Boettcher, A. L., 1978. Amphiboles in Andesite and Basalt: II. Stability as a Function of P-T-f H2O-f O2. American Mineralogists, 63(11–12): l074–1087
Aydin, F., Karsli, O., Sadiklar, M. B., 2003. Mineralogy and Chemistry of Biotites from Eastern Pontide Granitoid Rocks, NE-Turkey: Some Petrological Implications for Granitoid Magmas. Chem. Erde, 63(2): 163–182
Beane, R. E., 1974. Biotite Stability in the Porphyry Copper Environment. Economic Geology, 69(2): 241–256
Behrens, H., Gaillard, F., 2006. Geochemical Aspects of Melts: Volatiles and Redox Behaviour. Elements, 2(5): 275–280
Burkhard, D. J. M., 1993. Biotite Crystallization Temperatures and Redox States in Granitic Rocks as Indicator for Tectonic Setting. Geol. en Mijnb., 71(4): 337–349
Czamanske, G. K., Dillet, B., 1988. Alkali Amphibole, Tetrasilicic Mica and Sodic Pyroxene in Peralkaline Siliceous Rocks, Questa Caldera, New Mexico. American Journal of Science, 288-A: 358–392
Desikachar, S. V., 1974. A Review of the Tectonic and Geological History of Eastern India in Terms of Plate Tectonics Theory. Journal of Geological Society, India, 15: 137–149
Dodge, F. C. W., Moore, J. G., 1968. Occurrence and Composition of Biotites from the Cartridge Pass Pluton of the Sierra Nevada Batholith, California. Geol. Surv. Res. 1968. Prof. Pap. USGS, 600-B: B6–B10
Dwivedi, A. K., Pandey, U. K., Murugan, C., et al., 2011. Geochemistry and Geochronology of A-Type Barabazar Granite: Implications on the Geodynamics of South Purulia Shear Zone, Singhbhum Craton, Eastern India. Journal of Geological Society, India, 77(6): 527–538
Dymek, R. F., 1983. Titanium, Aluminium and Interlayer Cation Substitutions in Biotite from High Grade Gneisses, West Greenland. American Mineralogists, 68: 880–899
Ewart, A., 1979. A Review of the Mineralogy and Chemistry of Tertiary-Recent Dacitic, Latitic, Rhyolitic and Related Salic Volcanic Rocks. In: Fred, B., ed., Trondhjemites, Dacites, and Related Rocks. Springer-Verlag, Berlin. 12–101
Foster, M. D., 1960. Interpretation of the Composition of Trioctahedral Micas. U.S.G.S. Prof. Paper, 354B: 1–49
Haslam, H. W., 1968. The Crystallization of Intermediate and Acid Magmas at Ben Nevis, Scotland. Journal of Petrology, 9(1): 84–104
Hecht, L., 1994. The Chemical Composition of Biotite as an Indicator of Magmatic Fractionation and Metasomatism in Sn-Specialised Granites of the Fichtelgebirge (NW Bohemian Massif, Germany). In: Seltmann, R., Kämpf, H., Möller, P., eds., Metallogeny of Collisional Orogens. Czech Geol. Surv., Praha., 295–300
Helmy, H. M., Ahmed, A. F., El Mahallawi, M. M., et al., 2004. Pressure, Temperature and Oxygen Fugacity Conditions of Calc-Alkaline Granitoids, Eastern Desert of Egypt, and Tectonic Implications. Journal of African Earth Science, 38(3): 255–268
Hossain, I., Tsunogae, T., Rajesh, H. M., 2009. Geothermobarometry and Fluid Inclusions of Dioritic Rocks in Bangladesh: Implications for Emplacement Depth and Exhumation Rate. Journal of Asian Earth Science, 34(6): 731–739
Hossain, I., Tsunogae, T., Rajesh, H. M., 2008. Petrogenetic Characterization of Palaeoproterozoic Basement Rocks from Bangladesh: A Remnant of Magmatism Associated with the Columbia Supercontinent Amalgamation. Geochimica et Cosmochimica Acta, 72: A394
Hossain, I., Tsunogae, T., 2008. Fluid Inclusion Study of Pegmatite and Aplite Veins of Palaeoproterozoic Basement Rocks in Bangladesh: Implications for Magmatic Fluid Compositions and Crystallization Depth. Journal of Mineralogical and Petrological Sciences, 103: 121–125
Hossain, I., Tsunogae, T., Rajesh, H. M., et al., 2007. Palaeoproterozoic U-Pb SHRIMP Zircon Age from Basement Rocks in Bangladesh: A Possible Remnant of the Columbia Supercontinent. Comtes Rendus Geoscience, 339(16): 979–986
Jacobs, D. C., Parry, W. T., 1979. Geochemistry of Biotite in the Santa Rita Porphyry Copper Deposit, New Mexico. Economic Geology, 74(4): 860–887
Kawakatsu, K., Yamaguchi, Y., 1987. Successive Zoning in Amphiboles during Progressive Oxidation in the Daito-Yokota Granitic Complex, Sanin Belt, Southwest Japan. Geochimica et Cosmochimica Acta, 51(3): 535–540
Khan, A. A., Chouhan, R. K. S., 1996. The Crustal Dynamics and the Tectonic Trends in the Bengal Basin. Journal of Geodynamics, 22(3–4): 267–286
Kumar, S., Rino, V., 2006. Mineralogy and Geochemistry of Microgranular Enclaves in Palaeoproterozoic Malanjkhand Granitoids, Central India: Evidence of Magma Mixing, Mingling, and Chemical Equilibration. Contributions to Mineralogy and Petrology, 152(5): 591–609
Lalonde, A. E., Bernard, P., 1993. Composition and Color of Biotite from Granites: Two Useful Properties in the Characterization of Plutonic Suites from the Hepburn Internal Zone of Wopmay Orogen, Northwest Territories. Canadian Mineralogists, 31: 203–217
LaLonde, A. E., Martin, R. F., 1983. The Baie-Des-Moutons Syenitic Complex, La Tabatiere, Qubec, II. The Ferromagnesian Minerals. Canadian Mineralogists, 21: 81–91
Martel, C., Pichavant, M., Holtz, F., et al., 1999. Effects of f O2 and H2O on Andesite Phase Relation between 2 and 4 kbar. Journal of Geophysical Research, 104(B12): 29453–29470
Martin, R. F., 2007. Amphiboles in the Igneous Environment. Reviews of Mineralogy and Geochemistry, 67: 323–358
Mishra, B., Saravanan, C. S., Bhattacharya, A., et al., 2007. Im plications of Super Dense Carbonic and Hypersaline Fluid Inclusions in Granites from the Ranchi Area, Chottanagpur Gneissic Complex, Eastern India. Gondwana Research, 11(4): 504–515
Moore, G., Vennemann, T., Carmichael, I. S. E., 1998. An Empirical Model for the Solubility of H2O in Magmas to 3 Kilobars. American Mineralogists, 83: 36–42
Mueller, R. F., 1972. Stability of Biotite: A Discussion. American Mineralogists, 57(1–2): 300–316
Newman, S., Lowenstern, J. B., 2002. VolatileCalc: A Silicate Melt-H2O-CO2 Solution Model Written in Visual Basic for Excel. Computer & Geosciences, 28: 597–604
O’Neill, H. St. C., Pownceby, M. L., 1993. Thermodynamic Data from Redox Reactions at High Temperatures. I. An Experimental and Theoretical Assessment of the Electrochemical Method Using Stabilized Zirconia Electrolytes, with Revised Values for the Fe-“FeO”, Co-CoO, Ni-NiO, and Cu-Cu2O Oxygen Buffers, and New Data for the W-WO2 Buffer. Contributions to Mineralogy and Petrology, 114(3): 296–314
Reimann, K. U., 1993. Geology of Bangladesh. Gebruder Borntraeger, Berlin-Stuttgart. 160
Ridolfi, F., Renzulli, A., Puerini, M., 2010. Stability and Chemical Equilibrium of Amphibole in Calc-Alkaline Magmas: An Overview, New Thermobarometric Formulations and Application to Subduction-Related Volcanoes. Contributions to Mineralogy and Petrology, 160(1): 45–66
Ridolfi, F., Puerini, M., Renzulli, A., et al., 2008. The Magmatic Feeding System of El Reventador Volcano (Sub-Andean Zone, Ecuador) Constrained by Texture, Mineralogy and Thermobarometry of the 2002 Erupted Products. Journal of Volcanology and Geothermal Research, 176(1): 94–106
Rieder, M., 2001. Mineral Nomenclature in the Mica Group: The Promise and the Reality. European Journal of Mineralogy, 13: 1009–1012
Scaillet, B., Evans, B. W., 1999. The 15 June 1991 Eruption of Mount Pinatubo: I, Phase Equilibria and Pre-Eruption P-Tf O2-fH2 Conditions of the Dacite Magmas. Journal of Petrology, 40: 381–411
Selby, D., Nesbitt, B. E., 2000. Chemical Composition of Biotite from the Casino Porphyry Cu-Au-Mo Mineralization, Yukon, Canada: Evaluation of Magmatic and Hydrothermal Fluid Chemistry. Chemical Geology, 171(1–2): 77–93
Solie, D. N., Su, S. C., 1987. An Occurrence of Barich Micas from the Alaska Range. American Mineralogists, 72: 995–999
Speer, J. A., 1987. Evolution of Magmatic AFM Mineral Assemblages in Granitoid Rocks: The Hornblende+Melt=Biotite Reaction in the Liberty Hill Pluton, South Carolina. American Mineralogists, 7: 863–878
Speer, J. A., 1984. Micas in Igneous Rocks. Reviews in Mineralogy and Geochemistry, 13(1): 299–356
Tahmasbi, Z., Khalili, M., Ahmadi-Khalaji, A., 2009. Thermobarometry of the Astaneh Pluton and Its Related Subvolcanic Rocks (Sanandaj-Sirjan Zone, Western Iran). Journal of Applied Science, 9(5): 874–882
Walch, J. N., 1975. Clinopyroxenes and Biotites from the Centre III Igneous Complex, Ardnamurchan, Argyllashire. Mineralogical Magazine, 40: 335–345
Wones, D. R., 1989. Significance of the Assemblage Titanite+ Magnetite+Quartz in Granitic Rocks. American Mineralogists, 74(7–8): 744–749
Wones, D. R., Eugster, H. P., 1965. Stability of Biotite: Experiment, Theory, and Application. American Mineralogists, 50(9): 1228–1272
Yavuz, F., Öztaş, T., 1997. BIOTERM-A Program for Evaluating and Plotting Microprobe Analyses of Biotite from Barren and Mineralized Magmatic Suites. Computer & Geosciences, 23(8): 897–907
Yavuz, F., Gültekin, A. H., Örgün, Y., et al., 2002. Mineral Chemistry of Barium- and Titanium-Bearing Biotites in Calc-Alkaline Volcanic Rocks from the Mezitler Area (Balιkesir-Dursunbey), Western Turkey. Geochemical Journal, 36: 563–580