Provenance, diagenesis, tectonic setting, and geochemistry of Hawkesbury Sandstone (Middle Triassic), southern Sydney Basin, Australia

The Hawkesbury Sandstone is an important groundwater reservoir in the southern part of the Sydney Basin, Australia. However, its diagenesis and provenance and its impact in reservoir quality are virtually unknown. The present study aims to reconstruct the parent rock assemblages of the Hawkesbury Sandstone, their tectonic provenance, and the physiographic conditions under which these sediments were deposited. Samples from the EAW 18a and EDEN 115 field representing the Middle Triassic Hawkesbury Sandstone were studied using a combination of petrographic, mineralogical, and geochemical techniques. The Hawkesbury Sandstone is yellowish brown in color, siliceous, and partly calcareous; it originated as sands were deposited in fluvial channels. Texturally, Hawkesbury Sandstone is medium- to coarse-grained, mature, and moderately well sorted. Scarcity of feldspars indicates that the rock is extensively recycled from a distant source. Hawkesbury Sandstone has an average framework composition of Q92.07F0.31R7.62, and 95.9% of the quartz grains are monocrystalline. The Hawkesbury Sandstone is mostly quartz arenites with subordinate sublithic arenites, and bulk-rock geochemistry supports the petrographic results. Petrographic and geochemical data of the sandstones indicate that they were derived from craton interior to quartzose recycled sedimentary rocks and deposited in a passive continental margin of a syn-rift basin. The cratonic Lachlan Orogen is the main source of Hawkesbury Sandstone. The chemical index of alteration, plagioclase index of alteration, and chemical index of weathering values (3.41-87.03) of the Hawkesbury Sandstone indicate low-moderate to high weathering, either of the original source or during transport before deposition, and may reflect low-relief and humid climatic conditions in the source area. Diagenetic features include compaction: kaolinite, silica, mixed-layer clays, siderite, illite, and ankerite cementation with minor iron-oxide, dolomite, chlorite, and calcite cements. Silica dissolution, grain replacement, and carbonate dissolution greatly enhance the petrophysical properties of many sandstone samples.

Provenance, diagenesis, tectonic setting, and geochemistry of Hawkesbury Sandstone (Middle Triassic), southern Sydney Basin, Australia

The Hawkesbury Sandstone is an important groundwater reservoir in the southern part of the Sydney Basin, Australia. However, its diagenesis and provenance and its impact in reservoir quality are virtually unknown. The present study aims to reconstruct the parent rock assemblages of the Hawkesbury Sandstone, their tectonic provenance, and the physiographic conditions under which these sediments were deposited. Samples from the EAW 18a and EDEN 115 field representing the Middle Triassic Hawkesbury Sandstone were studied using a combination of petrographic, mineralogical, and geochemical techniques. The Hawkesbury Sandstone is yellowish brown in color, siliceous, and partly calcareous; it originated as sands were deposited in fluvial channels. Texturally, Hawkesbury Sandstone is medium- to coarse-grained, mature, and moderately well sorted. Scarcity of feldspars indicates that the rock is extensively recycled from a distant source. Hawkesbury Sandstone has an average framework composition of Q92.07F0.31R7.62, and 95.9% of the quartz grains are monocrystalline. The Hawkesbury Sandstone is mostly quartz arenites with subordinate sublithic arenites, and bulk-rock geochemistry supports the petrographic results. Petrographic and geochemical data of the sandstones indicate that they were derived from craton interior to quartzose recycled sedimentary rocks and deposited in a passive continental margin of a syn-rift basin. The cratonic Lachlan Orogen is the main source of Hawkesbury Sandstone. The chemical index of alteration, plagioclase index of alteration, and chemical index of weathering values (3.41-87.03) of the Hawkesbury Sandstone indicate low-moderate to high weathering, either of the original source or during transport before deposition, and may reflect low-relief and humid climatic conditions in the source area. Diagenetic features include compaction: kaolinite, silica, mixed-layer clays, siderite, illite, and ankerite cementation with minor iron-oxide, dolomite, chlorite, and calcite cements. Silica dissolution, grain replacement, and carbonate dissolution greatly enhance the petrophysical properties of many sandstone samples.

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  • Aalto KR (1972). Diagenesis of orthoquartzites near Bogota Columbia. J Sediment Petrol 42: 330–340.
  • Abouessa A, Morad S (2009). An integrated study of diagenesis and depositional facies in tidal sandstones: Hawaz Formation (Middle Ordovician), Murzuq Basin, Libya. J Petrol Geol 32: 39–66.
  • Abu-Zeid MM, Amer KM, El-Mohammady RA (1989). Petrology, mineralogy and provenance of sandstones of “Nubia” facies in west central Sinai. Earth Science Series 3, Middle East Research Centre, Ain Shams University: 20–34.
  • Abu-Zeid, MM, Amer KM, Yanni NN, El-Wekeil SS (1991). Petrology, mineralogy and sedimentation of the Paleozoic sequence of Gabal Qattar, Wadi Feiran, Sinai, Egypt. J Geol 34: 145–169.
  • Agrawal S, Guevara M, Verma SP (2004). Discriminant analysis applied to establish major element field boundaries for tectonic varieties of basic rocks. Int Geol Rev 46: 575–594.
  • Ahmad I, Chandra R (2013). Geochemistry of loess-paleosol sediments of Kashmir Valley, India: provenance and weathering. J Asian Earth Sci 66: 73–89.
  • Ahmed AHM, Bhat GM (2006). Petrofacies, provenance and diagenesis of the dhosa sandstone member (Chari Formation) at Ler, Kachchh sub-basin, Western India. J Asian Earth Sci 27:
  • Akarish AIM, El-Gohary AM (2008). Petrography and geochemistry of lower Paleozoic sandstones, East Sinai, Egypt: implications for provenance and tectonic setting. J Afr Earth Sci 52: 43–54.
  • Al-Habri OA, Khan MM (2008). Provenance, diagenesis, tectonic setting and geochemistry of Tawil sandstone (Lower Devonian in central Saudi Arabia). J Asian Earth Sci 33: 278–287.
  • Ali AD, Tuner P (1982). Authigenic K-feldspar in the Bromsgrove Sandstone Formation (Triassic) of central England. J Sediment Petrol 52: 187–198.
  • Amer KM, Abu-Zeid MM, El-Mohammady RA (1989). Particle-size distribution and depositional environment of the sandstones of “Nubia” facies in west central Sinai. Earth Science Series 3, Middle East Research Centre, Ain Shams University: 146–160.
  • Amireh BS (1991). Mineral composition of the Cambrian-Cretaceous Nubian series of Jordan: provenance, tectonic setting and climatological implication. Sediment Geol 71: 99–119.
  • Armstrong-Altrin JS, Lee YI, Kasper-Zubillaga, JJ, Carranza- Edwards A, Garcia D, Eby N, Balaram V, Cruz-Ortiz NL (2012). Geochemistry of beach sands along the Western Gulf of Mexico, Mexico: implication for provenance. Chem Erde Geochem 72: 345–362.
  • Armstrong-Altrin JS, Lee YI, Verma SP, Ramasamy S (2004). Geochemistry of sandstones from the Upper Miocene Kudankulam Formation, southern India: implications for provenance, weathering, and tectonic setting. J Sediment Res 74: 285–297.
  • Armstrong-Altrin JS, Nagarajan R, Madhavaraju J, Rosalez-Hoz L, Lee YI, Balaram V, Cruz-Martinez A, Avila-Ramirez G (2013). Geochemistry of the Jurassic and upper Cretaceous shales from the Molango Region, Hidalgo, Eastern Mexico: implications of source-area weathering, provenance, and tectonic setting. C R Geosci 345: 185–202.
  • Armstrong-Altrin JS, Verma SP (2005). Critical evaluation of six tectonic setting discrimination diagrams using geochemical data of Neogene sediments from known tectonic setting. Sediment Geol 177: 115–129.
  • Ashley GM, Duncan IJ (1977). The Hawkesbury Sandstone: a critical review of proposed environmental models. Journal of the Geological Society of Australia 24: 117–119.
  • Bakkiaraj R, Nagendra, Nagarajan R, Armstrong-Altrin JS (2010). Geochemistry of sandstones from the Upper Cretaceous Sillakkudi Formation, Cauvery basin, southern India: implication for provenance. J Geol Soc India 76: 453–467.
  • Bamberry WJ (1992). Stratigraphy and sedimentology of the Late Permian Illawarra Coal Measures, Southern Sydney Basin, New South Wales. PhD, University of Wollongong, Wollongong, Australia.
  • Basu A (1976). Petrology of Holocene fluvial sand derived from plutonic source rocks: implications to palaeoclimatic interpretation. J Sediment Petrol 46: 694–709.
  • Basu A, Young S, Suttner LJ, James WC, Mack CH (1975). Re-evaluation of the use of Undulatory extinction and polycrystallinity in detrital quartz for provenance interpretation. J Sediment Petrol 45: 873–882.
  • Bhatia MR (1983). Plate tectonics and geochemical composition of sandstones. J Geol 91: 611–627.
  • Bhatia MR, Crook KAW (1986). Trace element characteristics of greywackes and tectonic setting discrimination of sedimentary basins. Contrib Mineral Petr 92: 181–193.
  • Bjorlykke K (1983). Diagenic reactions in sandstones. In: Parker A, Sellwood BW, editors. Sediment Diagenesis. Dordrecht, the Netherlands: Reidel Publishing, pp. 169–213.
  • Bjİrlykke K, Aagaard P, Dypvik H, Hastings AS, Harper DS (1986). Diagenesis and reservoir properties of Jurassic sandstones from the Haltenbanken area, offshore mid-Norway. In: Spencer AM, Holter E, Cambell CJ, Hanslien PHH, Nysæther E, Ormaasen EG, editors. Habitat of Hydrocarbons of the Norwegian Continental Shelf. London, UK: Graham and Trotman, pp. 275–276.
  • Bjİrlykke K, Egeberg PK (1993). Quartz cementation in sedimentary basins. AAPG Bull 77: 1538–1548.
  • Blatt H, Middleton G, Murray R (1980). Origin of Sedimentary Rocks. 2nd ed. Englewood Cliffs, NJ, USA: Prentice Hall.
  • Boles JR, Franks SG (1979). Clay diagenesis in Wilcox sandstones of southwest Texas: implications of smectite diagenesis on sandstone cementation. J Sediment Petrol 49: 55–70.
  • Burley SD, Kantorowicz JD (1986). Thin section and SEM textural criteria for the recognition of cement-dissolution porosity in sandstones. Sedimentology 33: 587–604.
  • Chamley H (1990). Clay Sedimentology. Berlin, Germany: Springer- Verlag.
  • Conaghan PJ (1980). The Hawkesbury Sandstone: gross characteristics and depositional environment. In: Herbert C, Helby R, editors. A Guide to the Sydney Basin. Bulletin No. 26. Maitland, Australia: Geological Survey of New South Wales, pp. 188–253.
  • Conaghan PJ, Jones JG (1975). The Hawkesbury Sandstone and the Brahmaputra: a depositional model for continental sheet sandstones. Journal of the Geological Society of Australia 22:
  • Conolly JR (1969). Models for Triassic deposition in the Sydney Basin. Special Publication, Journal of the Geological Society of Australia 2: 209–223.
  • Conolly JR, Ferm JC (1971). Permo-Triassic sedimentation patterns, Sydney Basin, Australia. AAPG Bull 55: 2018–2032.
  • Cox R, Lowe DR, Cullers RL (1995). The influence of sediment recycling and basement composition on evolution of mudrock chemistry in the southwestern United States. Geochim Cosmochim Ac 59: 2919–2940.
  • Dapples EC (1979). Diagenesis in sandstones. In: Larsen G, Chinlinger GV, editors. Developments in Sedimentology, Vol. 25, Part A. Amsterdam, the Netherlands: Elsevier, pp. 31–97.
  • Davis JC (1986). Statistics and Data Analysis in Geology. New York, NY, USA: John Wiley & Sons.
  • Dehghani MH (1994). Sedimentology, genetic stratigraphy and depositional environment of the Permo-Triassic Succession in the Southern Sydney Basin, Australia. PhD, University of Wollongong, Wollongong, Australia.
  • Dickinson WR (1970). Interpreting detrital modes of greywacke and arkose. J Sediment Petrol 40: 695–707.
  • Dickinson WR, Beard LS, Brakenridge GR, Erjavec, JL, Ferguson, RC, Inman KF, Knepp RA, Lindberg FA, Ryberg PT (1983). Provenance of North American Phanerozoic sandstones in relation to tectonic setting. J Geol Soc America 94: 222–235.
  • Dickinson WR, Suczek CA (1979). Plate tectonics and sandstone compositions. AAPG Bull 63: 2164–2182.
  • Dott RH (1964). Wackes, greywacke and matrix: what approach to immature sandstone classification. J Sediment Petrol 34: 625– 632.
  • Dutta PK (1987). Origin of rarity of first cycle quartzarenite (abstract). AAPG Bull 71: 551.
  • Dutton SP (1993). Influence of provenance and burial history on diagenesis of Lower Cretaceous Frontier Formation sandstones, Green River Basin, Wyoming. J Sediment Petrol 63: 665–667.
  • Dutton SP, Diggs TN (1990). History of quartz cementation in the Lower Cretaceous Travis Peak Formation, East Texas. J Sediment Petrol 60: 191–202.
  • El-ghali MA, Morad S, Mansburg H, Miguel AC, Sirat M Ogle (2009). Diagenetic alterations to marine transgression and regression in fluvial and shallow marine sandstones of the Triassic Buntsandstein and Keuper sequence, the Paris basin, France. Mar Petrol Geol 26: 289–309.
  • Fedo CM, Nesbitt HW, Young GM (1995). Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols with implications for paleoweathering conditions and provenance. J Geol 23: 921–924.
  • Folk RL (1974). Petrology of Sedimentary Rocks. Austin, TX, USA: Hemphill Publication Co.
  • Franzinelli E, Potter PE (1983). Petrology, chemistry and texture of modern river sands, Amazon River System. J Geol 91: 23–39.
  • Gazzi P (1966). Le arenarie del flysch sopracretaceo dell’Appennino modensese: correlazioni con il flysch di Monghidoro. Mineralogica et Petrographica Acta 12: 69–97 (in Italian).
  • Gentz ML (2006). A pre-mining study of the Hawkesbury Sandstone and aquifer characeristics of potential longwall mining area, Appin area 3. Bachelor of Environmental Science Thesis, University of Wollongong, Wollongong, Australia.
  • Grevenitz P, Carr P, Hutton A (2003). Origin, alteration and geochemical correlation of Late Permian airfall tuffs in coal measures, Sydney Basin, Australia. Int J Coal Geol 55: 27–46.
  • Hawkins PJ (1978). Relationship between diagenesis, porosity reduction and oil replacement in Late Carboniferous sandstone reservoirs, Bothamsall oil Şeld, E. Midlands. J Geol Soc London 135: 7–24.
  • Herbert C (1980). Wianamatta Group and Mittagong Formation. In: Herbert C, Helby R, editors. A Guide to the Sydney Basin. Bulletin No. 26. Maitland, Australia: Geological Survey of New South Wales, pp. 254–272.
  • Herron MM (1988). Geochemical classification of terrigenous sands and shales from core or log data. J Sediment Petrol 58: 820–829.
  • Hindrix MS (2000). Evaluation of Mesozoic sandstone composition, southern Junggar, northern Tarim and western Turran basins, northwest China: a detrital record of the ancestral Tian Shan. J Sediment Res 70: 520–532.
  • Hofer G, Wagreich M, Neuhuber S (2013). Geochemistry of fine- grained sediments of the Upper Cretaceous to Paleogene Gosau Group (Austria, Slovakia): implications for paleoenvironmental and provenance studies. Geosci Front 4: 449–468.
  • Holail HM, Moghazi AM (1998). Provenance, tectonic setting and geochemistry of greywackes and siltstones of the Late Precambrian Hammamat Group, Egypt. Sediment Geol 116: 227–250.
  • Houseknecht DW (1988). Intergranular pressure solution in four quartzose sandstones. J Sediment Petrol 58: 228–246.
  • Hower J, Eslinger EV, Hower ME, Perry EA (1976). Mechanism of burial metamorphism of argillaceous sediments: 1. Mineralogical and chemical evidence. AAPG Bull 87: 725–737.
  • Ingersoll RV, Bulard TF, Ford RL, Grimn JP, Pickle JP, Sares SW (1984). The effect of grain size on detrital modes: a text of the Gazzi-Dickinson Point Counting method. J Sediment Petrol 54: 103–116.
  • Ingersoll RV, Suczek CA (1979). Petrology and provenance of Neogene sand from Nicobar and Bengal fans, DSDP sites 211 and 218. J Sediment Petrol 49: 1217–1228.
  • Jafarzadeh M, Harami RM, Amini A, Mahboubi A, Farzaneh F (2013). Geochemical constraints on the provenance of Oligocene- Miocene siliciclastic deposits (Zivah Formation) of NW Iran: implications for the tectonic evolution of the Caucasus. Arab J Geosci 7: 4245–4263.
  • Jafarzadeh M, Hosseini-Barzi M (2008). Petrography and geochemistry of Ahwaz Sandstone Member of Asmari Formation, Zagros, Iran: implications on provenance and tectonic setting. Rev Mex de Cien Geol 25: 247–260.
  • James WC, Mack GH, Suttner LJ (1981). Relative alteration of microcline and sodic plagioclase in semiarid and humid climates. J Sediment Petrol 51: 151–164.
  • Jin Z, Li F, Cao J, Wang S, Yu J (2006). Geochemistry of Daihai Lake sediments, Inner Mongolia, north China: implications for provenance, sedimentary sorting and catchment weathering. Geomorphology 80: 147–163.
  • Johnson MD (2006). Solutional weathering of the Hawkesbury Sandstone and cliff instability. Bachelor of Environmental Science Thesis, University of Wollongong, Wollongong, Australia.
  • Keller WD (1956). Clay minerals as influenced by environments of their formation. AAPG Bull 40: 2689–2710.
  • Khanchuk AI, Nevstruev VG, Berdnikov NV, Nechaev VP (2013). Petrochemical characteristics of carbonaceous shales in the eastern Bureya massif and their precious-metal mineralization. Russ Geol Geophys 54: 627–636.
  • Kim JC, Lee YI, Hisada KI (2007). Depositional and compositional controls on sandstone diagenesis, the Tetori Group (Middle Jurassic-Early Cretaceous), central Japan. Sediment Geol 195: 183–202.
  • Kroonenberg SB (1994). Effects of provenance, sorting and weathering on the geochemistry of fluvial sands from different tectonic and climatic environments. In: Proceedings of the 29th International Geological Congress, Part A, Kyoto, Japan, 1992. Utrecht, the Netherlands: VSP Publishing, pp. 69–81.
  • Laird MG (1972). Sedimentology of Greenland Group in the Paparoa Range, West Coast, South Island, New Zealand. J Geol Geophys 15: 372–393.
  • Le Bas MJ, Le Maitre RW, Streckeisen A, Zanettin B (1986). A chemical classification of volcanic rocks based on the total alkali-silica diagram. J Petrol 27: 745–750.
  • Lee YI, Lim DH (2008). Sandstone diagenesis of the Lower Cretaceous Sindong Group, Gyeongsang Basin, southeastern Korea: implications for compositional and paleoenvironmental controls. Island Arc 17: 152–171.
  • Lonnie TP (1982). Mineralogic and chemical composition of marine and nonmarine transitional clay beds on south shore of Long Island, New York. J Sediment Petrol 52: 529–536.
  • McBride EF (1963). A classiŞcation of common sandstones. J Sediment Petrol 33: 664–669.
  • McLennan SM, Hemming S, McDaniel DK, Hanson GN (1993). Geochemical approaches to sedimentation, provenance, and tectonics. GSA Special Papers 284: 21–40.
  • McLennan SM, Taylor SR, McCulloch MT, Maynard JB (1990). Geochemical and Nd-Sr isotopic composition of deep-sea turbidites: crustal evolution and plate tectonic associations. Geochim Cosmochim Ac 54: 2015–2050.
  • Miall AD, Jones BG (2003). Fluvial architecture of the Hawkesbury Sandstone (Triassic), near Sydney, Australia. J Sediment Res 73: 531–545.
  • Morad S (1998). Carbonate cementation in sandstones: distribution patterns and geochemical evolution. In: Morad S, editor. Carbonate Cementation in Sandstones. Gent, Belgium: International Association of Sedimentologists Special Publication, pp. 1–26.
  • Morad S, Ketzer JM, De Ros F (2000). Spatial and temporal distribution of diagenetic alterations in siliciclastic rocks: implications for mass transfer in sedimentary basins. Sedimentology 47: 95–120.
  • Nath BN, Kunzendorf H, Pluger WL (2000). Influence of provenance, weathering and sedimentary processes on the elemental ratio of the fine-grained fraction of the bed load sediments from the Vembanad Lake and the adjoining continental shelf, southwest Coast of India. J Sediment Res 70: 1081–1094.
  • Naughton JJ, Terada K (1954). Effect of eruption of Hawaiian volcanoes on the composition and carbon isotopic composition of associated volcanic and fumarolic gases. Science 120: 580– 581.
  • Nesbitt HW, Fedo CM, Young GM (1997). Quartz and feldspar stability, steady and non-steady-state weathering, and petrogenesis of siliciclastic sands and muds. J Geol 105: 173– 192.
  • Nesbitt HW, Young GM (1982). Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature 299: 715–717.
  • Nesbitt HW, Young GM (1984). Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations. Geochim Cosmochim Ac 48: 1523–1534.
  • Nowrouzi Z, Moussavi-Harami R, Mahboubi A, Gharaie MHM, Ghaemi F (2013). Petrography and geochemistry of Silurian Niur sandstones, Derenjal Mountains, East Central Iran: implications for tectonic setting, provenance and weathering. Arab J Geosci 7: 2793–2813.
  • Osae S, Asiedu DK, Banoeng-Yakubo B, Koeberl C, Dampare SB (2006). Provenance and tectonic setting of Late Proterozoic Buem sandstones of southeastern Ghana: Evidence from geochemistry and detrital modes. J Asian Earth Sci 44: 85–96.
  • Pettijohn FJ (1963). Chemical Composition of Sandstones-Excluding Carbonate and Volcanic Sands. Reston, VA, USA: USGS Professional Paper.
  • Pettijohn FJ (1975). Sedimentary Rocks. 2nd ed. New York, NY, USA: Harper and Row.
  • Pettijohn FJ (1984). Sedimentary Rocks. 3rd ed. New Delhi, India: CBS Publishers & Distributors.
  • Pettijohn FJ, Potter PE, Siever R (1972). Sand and Sandstones. 1st ed. New York, NY, USA: Springer-Verlag.
  • Pettijohn FJ, Potter PE, Siever R (1987). Sand and Sandstones. 2nd ed. New York, NY, USA: Springer-Verlag.
  • Potter PE (1978). Petrology and chemistry of modern Big River sands. J Geol 86: 423–449.
  • Retallack GJ (1999). Postapocalyptic greenhouse paleoclimate revealed by earliest Triassic paleosols in the Sydney Basin, Australia. Geol Soc Am Bull 111: 52–70.
  • Rodrigo DL, Luiz FDR (2002). The role of depositional setting and diagenesis on the reservoir quality of Devonian sandstones from the Solimones Basin, Brazilian Amazonia. Mar Petrol Geol 19: 1047–1071.
  • Rollinson HR (1993). Using Geochemical Data: Evaluation, Presentation, Interpretation. London, UK: Longman.
  • Roser BP, Cooper RA, Nathan S, Tulloch AJ (1996). Reconnaissance sandstone geochemistry, provenance, and tectonic setting of the lower Paleozoic terranes of the West Coast and Nelson, New Zealand. New Zealand J Geol Geophys 39: 1–16.
  • Roser BP, Korsch RJ (1986). Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio. J Geol 94: 635–650.
  • Roser BP, Korsch RJ (1988). Provenance signatures of sandstone- mudstone suites determined using discrimination function analysis of major element data. Chem Geol 67: 119–139.
  • Rust BR, Jones BG (1987). The Hawkesbury Sandstone south of Sydney, Australia: Triassic analogue for the deposit of a large braided river. J Sediment Petrol 57: 222–233.
  • Saunders AD, England RW, Reichow MK, White RV (2005). A mantle plume origin for the Siberian traps: uplift and extension in the West Siberian Basin, Russia. Lithos 79: 407–424.
  • Schwab FL (1975). Framework mineralogy and chemical composition of continental margin type sandstone. Geology 3: 487–490.
  • Selvaraj K, Chen CTA (2006). Moderate chemical weathering of subtropical Taiwan: constraints from solid-phase geochemistry of sediments and sedimentary rocks. J Geol 14: 101–116.
  • Shadan M, Hosseini-Barzi M (2013). Petrography and geochemistry of the Ab-e-Haji Formation in central Iran: implications for provenance and tectonic setting in the southern part of the Tabas block. Rev Mex Cien Geol 30: 80–95.
  • Spry AH (2000). The Hawkesbury Sandstone: its origins and later life. In: McNally GH, Franklin BJ, editors. Sandstone City: Sydney’s Dimension Stone and other Sandstone Geomaterials: Proceedings of a Symposium, University of Technology, Sydney, Australia.
  • Standard JC (1969). Hawkesbury Sandstone. Journal of the Geological Society of Australia 16: 407–417.
  • Sur KH, Lee YI, Hisada KI (2002). Diagenesis of the Lower Cretaceous Kanmon Group sandstones, SW Japan. J Asian Earth Sci 20: 921–935.
  • Suttner LJ, Basu A, Mack GH (1981). Climate and the origin of quartz arenites. J Sediment Petrol 51: 235–246.
  • Suttner LJ, Dutta PK (1986). Alluvial sandstone composition and paleoclimate, I. Framework mineralogy. J Sediment Petrol 56: 329–345.
  • Taylor JM (1950). Pore-space reduction in sandstones. AAPG Bull 34: 701–716.
  • Taylor SR, McLennan SM (1985). The Continental Crust: Its Composition and Evolution. Oxford, UK: Blackwell.
  • Trevena AS, Nash WP (1981). An electron microprobe study of detrital feldspar. J Sediment Petrol 51: 137–150.
  • Tsuzuki Y, Kawabe I (1983). Polymorphic transformations of kaolin minerals in aqueous solutions. Geochim Cosmochim Ac 47: 59–66.
  • Umar M, Friis H, Khan A, Kassi, AM, Kasi AK (2011). The effects of diagenesis on the reservoir characters in sandstones of the