سازوکار تشکیل سیلیس و دولومیت در سنگ‌های کربناتی ژوراسیک فوقانی (آکسفوردین – کیمریجین- تیتونین؟) در غرب بجنورد و جاجرم

[1] Dickson J. A. D., “Carbonate identification and genesis as revealed by staining”, Journal of Sedimentary Petrology 36 (1966) 441–505.

[2] Sibley D. F., Gregg J. M., “Classiffication of dolomite rock textures”, Journal of Sedimentary Petrology 57 (1987) 967–975.

[3] Flugel E., “Microfacies of Carbonate Rocks-Analysis, Interpretation and Application”, Springer, Berlin (2010) 967 pp.

[4] Tucker M. E., “Sedimentary Rocks in the Field”, 3rd edn. John Wiley & Sons Ltd, New York (2003) 249 pp.

[5] Kolodny Y., “The origin of cherts as members of high productivity sequences: Isotopic evidence. The Scientific Study of Flint and Chert”, In: (eds. G. de G Sieveking and M. B. Hart), (1986) 55–62.

[6] Bromley R. G., Ekdale A. A., “Flint and fabric in the European chalk. In The Scientific Study of Flint and Chert”, In: (eds. G. de G Sieveking and M. B. Hart), (1986) 71–82.

[7] Sharp, Z. D., Durakiewicz, T., Migaszewski, Z. M., Atudorei V. N., “Antiphase hydrogen and oxygen isotope periodicity in chert nodules”, Geochimica et Cosmochimica Acta 66 (2002) 2865–2873.

[8] Muttoni G., Kent D. V., “Widespread formation of cherts during the early Eocene climate optimum”, Palaeogeography, Palaeoclimatology, Palaeoecology 253 (2007) 348–362.

[9] Moore T. C., “Chert in the Pacific: Biogenic silica and hydrothermal circulation”, Palaeogeography, Palaeoclimatology, Palaeoecology 261(2008) 87–99.

[10] Akulov N. I., “Nodules in carbonaceous sediments of the Southern Tunguska Basin”, Lithology and Mineral Resources 41 (2006) 73–84.

[11] Simonson, B.M., “Sedimentology of cherts in the Early Proterozoic Wishart Formation, Quebec-newfoundland, Canada”, Sedimentology 32 (1985) 23-40.

[12] Meadows D., Davies R. J., “Predicting porosity reduction due to silica diagenesis using seismic reflection data”, Marine and Petroleum Geology 26 (2009) 1543–1553.

[12] Knauth L. P., Lowe D. R., “High Archean climatic temperature inferred from oxygen isotope geochemistry of cherts in the 3.5 Ga Swaziland Supergroup, South Africa”, Geol. Soc. Am. Bull. 115 (2003) 566-580.

[13] Weibel R., Friis H., Kazerouni A. M., Svendsen J. B., Stokkendal J., Poulsen M. L. K., Development of early diagenetic silica and quartz morphologies — Examples from the Siri Canyon, Danish North Sea” Sedimentary Geology 228 (2010) 151–170.

[14] Sugitani K., Yamamoto K., Adachi M., Kavabe I., Sugisaki R., “Archean cherts derived from chemical, biogenic and clastic sedimentation in shallow restricted basin:examples from the Gorge Greek Group in the Pilbara Block”, Sedimentology 45 (1998)1045-1-62.

[15] Girty G. H., Ridge D. L., Knaack C., Johnson D., Al-Riyami R. K., “Provenance and depositional setting of Paleozoic chert and argillite, Sierra Nevada, California”, Journal of Sedimentary Research 66 (1996) 107–18.

[16] Knauth L. P., “Origin and diagenetic history of cherts: An isotopic perspective. Isotopic Signatures and Sedimentary Rocks”, In: (eds. N. Clauer and S. Chaudhuri), Springer-Verlag, Berlin, Germany 43 (1992) 123–152.

[17] Frisia S.,. “Mechanisms of complete dolomitization in a carbonate shelf: comparison between the Norian Dolomia Principale (Italy) and the Holocene of Abu Dhabi sabkha”, In: Purser, B.H., Tucker, M., Zenger, D. (Eds.), Dolomites, a Volume in Honour of Dolomieu. Special Publication, International Association of Sedimentologists, 21 (1994) 55–74.

[18] Budd D. A., “Cenozoic dolomites of carbonate islands: their attributes and origin”, Earth Science Review. 42 (1997) 1–47.

[19] Reinhold C., “Multiple episodes of dolomitization and dolomite recrystallization during shallow burial in Upper Jurassic shelf carbonates: eastern Swabian Alb, southern Germany”, Sedimentary Geology 121 (1998) 71–95.

[20] Gregg J. M., Shelton K.L., “Dolomitization and dolomite neomorphism in the back reef facies of the Bonnettere and Davis Formations (Cambrian), southeastern Missouri”, Journal of Sedimentary Petrology 60 (1990) 549-562.

[21] Al-Aasm I. S., Packard J. J., “Stabilization of early-formed dolomite: a tale of divergence from two Mississippian dolomites”, Sedimentary Geology 131 (2000) 97-108.

[22] Johnson A. W., Shelton K. L., Greeg M. J., Somerville I. D., Wright W. R., Nagy Z. R., “Regional studies of dolomites and their included fluids: recognizing multiple chemically distinct fluids during the complex diagenetic history of Lower Carboniferous (Mississippian) rocks of the Irish Zn-Pb ore field”, Miner Petrol. 96 (2009) 1-18.

[23] Warren J., Dolomite: “occurrence, evolution and economically important associations”, Earth Science Review 52 (2000) 1–81.

[24] Machel H. G., “Concepts and models of dolomitization: a critical reappraisal”, In: Braithwaite, C. J. R., Rizzi G, Darke G, (Eds.), The Geometry and Petrogenesis of Dolomite Hydrocarbon Reservoirs. Geol. Soc. London Spec. Publ. 235(2004) 7–63.

[25] Choquette P. W., Hiatt E. E., “Shallow-burial dolomite cement: a major component of many ancient sucrosic dolomites”, Sedimentology 55 (2008) 423–460.

[26] Reeder, R. J., Prosky, J. L., “Compositional sector zoning in dolomite”, Journal of Sedimentary Petrology 56 (1986) 237–247.

[27] Jones B., Inside-out dolomite, Journal of Sedimentary Research 77 (2007) 539–551.

[28] Banner, J. L., “Application of the trace element and isotope geochemistry of strontium to studies of carbonate diagenesis”, Sedimentology 42 (1995) 805–824.

[29] Touir J., Soussi Mohamed, and Troudi, 2009, Polyphased dolomitization of a shoal-rimmed carbonate platform: example from the Middle Turonian Bireno dolomites of central Tunisia, Cretaceous Research v. 30, p. 785–804.

[30] Kirmaci M. Z., “Dolomitization of the late Cretaceous–Paleocene platform carbonates, Golkoy (Ordu), eastern Pontides, NE Turkey”, Sedimentary Geology 203 (2008) 289-306.

[31] Gregory R. T., In: Taylor Jr., H.P., O’Neil, J.R., Caplan, I.R. (Eds.). “Stable Isotope Geochemestry: a Tribute to Samuel Epstein, The Geochemical Society Special Publication”, 1. The Geochemical Society (1991) 65–76.

[32] Friedman I., O'Neil J. R., “Compilation of stable isotope fractionation factors of geochemical interest. Data of Geochemistry”, US Geol. Surv. Prof. Paper 440 (1977) 1–12.

[33] Bustillo M. A., Arribas M. E., Bustillo M., “Dolomitization and silicification in low-energy lacustrine carbonates (Paleogene, Madrid Basin, Spain)”, Sedimentary Geology 151 (2002) 107–126.

[34] Tucker M. E.,Wright V. P., “Carbonate Sedimentology”, Blackwell, Oxford. (1992) 482 pp.

[35] Machel H. G., Mountjoy E. W., “Chemistry and environments of dolomitization-a reappraisal”, Earth Science Reveiw 23 (1986) 175–222.

[36] Coniglio M., James N. P., Aissaoui D. M., “Dolomitization of Miocene carbonates, Gulf of Suez, Egypt”, Journal of Sedimentary Petrology 58 (1988) 100–119.

[37] Allan J. R., Wiggins W. D., “Dolomite reservoir geochemical techniques for evaluation, origin and distribution”, Am Assoc Petroleum Geol Bull Course Note Series 36 (1993) 129 p

[38] Padden M., Weissert H., Funk H., Schneider S., Gansner C., “Late Jurassic lithological evolution and carbon-isotope stratigraphy of the western Tethys”, Eclogae geol. Helv. 95 (2002) 333–346.

[39] Rasser M. W., Fenninger A., “Paleoenvironmental and diagenetic implications of δ18O and δ13C isotope ratios from the Upper Jurassic Plassen limestone (Northern Calcareous Alps, Austria)”, Géobios 35 (2002) 41–49.

[40] Lohmann, K.C., “Geochemical patterns of meteoric diagenetic systems and their application to studies of paleokarst”, In: James, N.P., Philip, W.C. (Eds.), Paleokarst. Springer, Berlin, (1988) 58–80.