ریزرخساره‌ها، محیط رسوبی و چینه‌نگاری سکانسی سازند آسماری در یال جنوبی تاقدیس کوه سیاه، شمال دهدشت، زاگرس

منابع

[1]   رحمانی، ع (1390) چینه­شناسی سازند آسماری در تاقدیس­های بنگستان و خویز و میدان نفتی پارسی، رساله­ی دکتری چینه­شناسی و فسیل­شناسی، دانشگاه اصفهان، 210ص.

[2]   کلنات، ب.، وزیری­مقدم، ح.، طاهری، ع (1389) زیست چینه نگاری و پالئواکولوژی سازند آسماری در جنوب غرب فیروز آباد. ریزرخساره­های رسوبی، جلد 3، صفحه71-84.

[3]   مطیعی، ه (1372) زمین­شناسی ایران، چینه­شناسی زاگرس. انتشارات سازمان زمین­شناسی کشور، 536 ص.

[4]   مؤسسه­ی جغرافیایی، کارتوگرافی گیتاشناسی (1384) اطلس راه­های ایران، مقیاس 1:100000.

[5]  Adams, T.D., Bourgeois, F (1967) Asmari biostratigraphy, Geological and Exploration, Iranian Offshore Oil Company Report. no. 1074, (unpublished).

[6]  Aguilera-Franco, N., Hernández-Romano, U (2004) Cenomanian-Turonianfacies succession in the Guerrero-Morelos Basin, Southern Mexico, Sedimentary Geology,v. 170 p. 135-162.

[7]  Allahkarampour Dill, M., Seyrafian, A. and Vaziri-Moghaddam, H (2010) The Asmari Formation, north of the Gachsaran (Dill anticline), southwest Iran:faciesanalysis, depositional environments and sequence stratigraphy, Carbonates and Evaporites.v. 25 p. 145–160.

[8]  Allahkarampour Dill, M., Seyrafian, A. and Vaziri-Moghaddam, H (2012) Palaeoecology of the Oligocene-Miocene Asmari Formation in the Dill Anticline, Zagros Basin, Iran, Neues. Jahrbuch für geology und paläontologie. V. 263 p. 167-184.

[9]  Amirshahkarami, M., Vaziri-Moghaddam, H. and Taheri, A (2007) Sedimentary faciesandSequencestratigeraphy of the Asmari Formation at the Chaman-Bolbol, Zagros Basin, Iran, Journalof Asian Earth Science.v. 29p. 947-959.

[10]   Amirshahkarami, M., Ghabishavi, A. and Rahmani, A (2010) Biostratigraphy and Paleoenvironment of the larger benthic foraminifera in wells section of the Asmari Formation from Rag-e-Safid oil fild,Zagros Basin, southwest Iran, Stratigraphy and Sedimentology Researches.v. 40p. 63-84.

[11]   Barattolo, F., Bassi, D. and Romero, R (2007) Upper Eocen larger foraminiferal-coralline algal facies from the Klokova Mountain, south continental Greece. Facies, 53, 361-375.

[12]   Beavington-Penney, S.J. and Racey, A (2004) Ecology of extant nummulitids and other larger benthic foraminifera, applications in palaeoenvironmental analysis. Earth-Science Reviews, 67, 219-265.

[13]   Brandano, M., Corda, L (2002) Nutrients, sea level and tectonics: constrains for the facies architecture of a Miocene carbonate ramp in central Italy, Terra Nova.v. 14p. 257-262.

[14]   Burchette, T.P. Wright, V.P(1992) Carbonate ramp depositional systems, Sedimentary Geology.v. 79p. 3-57.

[15]   Buxton, M.W.N., Pedley, H.M (1989) A standardized model for Thethyan Tertiary carbonate ramps, London, Journal of the Geological Society.v. 146p. 746-748.

[16]   Catuneanu, O., Abreu, V. Bhattacharya, J.P. Blum, M.D. Dalrymple, R.W. Eriksson, P.G. Fielding, C.R. Fisher, W.L. Galloway, W.E. Gibling, M.R. Giles, K.A. Holbrook, J.M. Jordan, R. Kendall, C.G.S.C. Macurda, B. Martinsen, O.J. Miall, A.D. Neal, J.E. Nummedal, D. Pomar, L. Posamentier, H.W. Pratt, B.R. Sarg, J.F. Shanley, K.W. Steel, R.J. Strasser, A. Tucker, M.E. and Winker, C (2009) Towards the standardization of sequence stratigraphy, Earth-Science Reviews.v. 92p. 1-33.

[17]   Catuneanu, O., Bhattacharya, J.P. Blum, M.D. Dalrymple, R.W. Eriksson, P.G. Fielding, C.R. Fisher, W.L. Galloway, W.E. Gianolla, P. Gibling, M.R. Giles, K.A. Holbrook, J.M. Jordan, R. Kendall, C.G.S.C. Macurda, B. Martinsen, O.J. Miall, A.D. Neal, J.E. Nummedal, D. Pomar, L. Posamentier, H.W. Pratt, B.R. Shanley, K.W. Steel, R.J. Strasser, A. and Tucker, M.E (2010) Sequence stratigraphy: common ground after three decades of development, Stratigraphy.v. 28 p. 21-33.

[18]   Corda, L., Brandana, M (2003) Aphotic zone carbonate production on a Miocene ramp, Central Apennines, Italy, Sedimentary Geology.v. 161 p. 55-70.

[19]   Cosovic, V., Drobne, K. and Moro, A (2004) Paleoenvironmental model for Eocene foraminiferallimestones of the Adriatic carbonate platform, Istrian Peninsula, Facies.v. 50 p. 61-75.

[20]   Dunham, R.J (1962) Classification of carbonate rocks according to their depositional texture, AAPG Memoir.v. 1p. 108-121.

[21]   Ehrenberg, S.N., Pickard, N.A.H., Laursen, G.V., Monibi, S., Mossadegh, Z.K., Svana,T.A., Agrawi, A.A.M., McArthur, J.M. and Thirlwall, M.F (2007) Strontium isotope stratigraphy of theAsmari Formation (Oligocene – Lower Miocene), SW Iran, Journal of Petroleum Geology.v. 30 p. 107-128.

[22]   Embry, A.F. and Klovan, J.E (1971) A Late Devonian reef tract on Northeastern Banks Island, NWT Canadian Petroleum Geology Bulletin. v.19 p. 730-781.

[23]   Flugel, E (2010) Microfacies Analysis of Carbonate Rocks, Interpretation and application, Springer-Verlag, Berlin, 976p.

[24]   Geel, T (2000) Recognition of stratigraphic sequence in carbonate platform and slope deposits, empirical models based on microfacies analysis Palaeogene deposits in southeastern Spain, Palaeogeography.p.211-238.

[25]   Hallock, P., Glenn, E.C (1986) Larger foraminifera: A tool for paleoenvironmental analysis of Cenozoic depositional facies, Palaios.v. 1 p. 55– 64.

[26]   Hardie, L.A (1986) Ancient carbonate tidal flate deposits, Quarterly Journal of the Colorado School of Mines. v. 81 p. 37-57.

[27]   Hernández-Romano, U (1999) Facies stratigraphy and diagenesis of the Cenomanian-Turonian of the Guerrero-Morelos platform, southern Mexico, United Kingdom, University of Reading, Postgraduate Research Institute for Sedimentology, Ph.D, Thesis, 322p.

[28]   Hottinger, L (1997) Shallow bentihic foraminiferal assembelages as signals for depth of their deposition and their limitations, Geology France.v. 168 p. 491–505.

[29]   James, G.A. Wynd, J.G (1965) Stratigraphic nomenclature of Iranian Oil Consortium Agreement Area, AAPG Bulletin.v. 49 p. 2182-2245.

[30]   Lasemi, Y (1995) Platform carbonates of the Upper Jurassic Mozduran Formation in the KopehDagh Basin, NE Iran-facies, palaeoenvironments and sequences, Sedimentary Geology. v. 99 p. 151-164.

[31]   Mossadegh, Z.K., Haig, D.W., Allan, T., Adabi, M.H. and Sadeghi, A (2009) Salinity changes during Late Oligocene to Early Miocene Asmari Formation deposition, Zagros Mountains,Iran, Palaeogeography, Palaeoclimatology, Palaeoecology.v. 272 p.17-36.

[32]   Nebelsick, J.H., Rasswe, M. and Bassi, D (2005) Facies dynamic in Eocene to Oligocene Circumalpine carbonates, Facies. v. 51 p. 197–216.

[33]   Pomar, L (2001a) Types of carbonate platforms: a genetic approach, Basin Research. v.13 p. 313-334.

[34]   Pomar, L (2001b) Ecological control of sedimentary accommodation, evolution from a carbonate ramp to rimmed shelf, Upper Miocene, Balearic Islands, Palaeogeography, Palaeoclimatology, Palaeoecology. v. 175 p. 249-272.

[35]   Rahmani, A., Vaziri-Moghaddam, H., Taheri, A. and Ghabeishavi, A (2009) A model for the paleoenvironmetal distribution of larger foraminifera of Oligocene-Miocene carbonate rocks at Khaviz Anticline, Zagros Basin, SW Iran, Historical Biology. V. 21 p. 215-227.

[36]   Rasser, M., Scheibner, C. and Mutti, M (2005) A paleoenvironmental standard section for Early Ilerdian tropical carbonate factories, (Corbieres, France; Pyrenees, Spain): Facies. v. 51 p. 218-232.

[37]   37-Reiss, Z. Hottinger, L (1948) The Gulf of Aqaba: ecological micropaleontology, Springer, Berlin Heidelberg New York, 345p.

[38]   Sadeghi R., Vaziri-Moghaddam, H. and Taheri, A(2010) Microfacies and sedimentary environment of the Oligocene sequence (Asmari Formation) in Fars sub-basin, Zagros Mountains, southwest Iran, Springer-Verlag. v. 57 p. 431-446.

[39]   Steinhauff, D.M., and Walker, K.R (1996) Sequence stratigraphy of an apparently non-cyclic carbonate succession: recognizing subaerial exposure in largely subtidal, Middle Ordovician stratigraphic sequence in eastern Tennessee, in Witzka, G.A., Ludvingson, J.E., Day, B.J. (eds.), Paleozoic Sequence Stratigraphy, Views from the North American Craton, Geological Society of America, Special Paper. v. 306 p. 87-115.

[40]   Taheri, A., Vaziri-Moghaddam, H. and Seyrafian, A (2008) Relationships between foraminiferal assemblages and depositional sequences in Jahrum Formation, Ardal area (Zagros Basin, SW Iran), Historycal biology. V. 20 p. 191-201.

[41]   Thomas, A.N (1948) The Asmari limestone of southwest Iran. National Iranian Oil Company, Report 706, unpublished.

[42]   van Buchem, F.S.P., Allan, T.L., Laursen, G.V., Lotfpour, M., Moallemi, A., Monibi, S., Motiei, H., Pickard, N.A.H., Tahmasbi, A.R., Vedrenne, V. and Vincent, B (2010) Regional stratigraphic architecture and reservoir types of the Oligo-Miocene deposits in the Dezful Embayment (Asmari and Pabdeh Formations) SW Iran. Geological Society, London, Special Publications. v. 329 p. 219-263.

[43]   Vaziri-Moghaddam, H., Kimiagari, M. and Taheri, A (2006) Depositional environment and sequence stratigraphy of the Oligocene-Miocene Asmari Formation in SW Iran, Lali Area, Facies. v. 52 p. 41-51.

[44]   Vaziri-Moghaddam, H., Seyrafian, A., Taheri A. and Motiei, H (2010) Oligocene-Miocene ramp system (Asmari Formation) in the NW of the Zagros Basin, Iran: Microfacies, paleoenvironment and depositional sequence, Revista Mexicana de CienciasGeológicas. v. 27 p. 56-71.

[45]   Wilson, J.L (1975) Carbonate facies in geological history, New York, Springer-Verlag, 471p.