Al-Aasm I S, Lonnee J S, Clarke J. 2002. Multiple fluid flow events and the formation of saddle dolomite: Case studies from the Middle Devonian of the Western Canada Sedimentary basin. Mar Pet Geol, 19: 209-217
[22]
Miroshnichenko M L. 2004. Thermophilic microbial communities of deep-sea hydrothermal vents. Microbiology, 73: 1-13
[23]
Murray R W. 1994. Chemical criteria to identify the depositional environment of chert: General principles and application. Sediment Geol, 90: 213-232
[24]
Nader F H ,Garcia D, Parra T, et al. 2009. Reactive geochemical transport modeling of hydrothermal dolomite fronts: The case of Marjaba dolomite front (Jurassic, Lebanon). J Geochem Explor, 101: 74
[25]
Nader F H, Swennen R, Ellam R. 2004. Reflux stratabound dolostone and hydrothermal volcanism-associated dolostone: A two-stage dolomitization model (Jurassic, Lebanon). Sedimentology, 51: 339-360
[26]
Le Guerroué E, Allen P A, Crozzi A. 2006. Chemostratigraphic and sedimentological framework of the largest negative carbon isotopic excursion in Earth History: The Neoproterozoic Shuram formation (Nafun Group, Oman). Precambrian Res, 146: 68-92
[27]
Liou J G. 1971. Analcime equilibria. Lithos, 4: 389-402
[28]
López-Horgue M A, Iriarte E, Schr？der S, et al. 2010. Structurally controlled hydrothermal dolomites in Albian carbonates of the Ason Valley, Basque cantabrian basin, Northern Spain. Mar Pet Geol, 27: 1069-1092
[29]
Machel H G, Lonnee J. 2002. Hydrothermal dolomite-a product of poor definition and imagination. Sediment Geol, 152: 163-171
[30]
Marchig V, Gundlach H, Moller P. 1985. Some geological indicators for discrimination between Digenetic and Hydrothermal Metalliferous Sediments. Mar Geol, 50: 241-256
[31]
Palmer M R, Elderfield H. 1985. Sr isotope composition of sea water over the past 75 Myr. Nature, 314: 526-528
[32]
Qing H, Mountjoy E W. 1994. Formation of coarsely crystalline, hydrothermal dolomite reservoirs in the Presqu’ile Barrier, Western Canada sedimentary basin. AAPG Bull, 78: 55-77
[33]
Qing H, Mountjoy E W. 1992. Large-scale fluid flow in the middle devonian Presqu’ile barrier, Western Canada sedimentary basin. Geology, 20: 903-906
[34]
Rosenthal Y, Lam P, Boyle E A, et al. 1995. Authigenic cadmium enrichments in suboxic sediments: Precipitation and post depositional mobility. Earth Planet Sci Lett. 132: 99-111
[35]
Roy P D, Kloss W S. 2007. REE geochemistry of the recent playa sediments from the Thar desert, India: An implication to Playa Sediment Provenance. Chem Erde-Geochem, 67: 55-68
[36]
Sass E. 1965. Dolomite-calcite relationships in seawater: Theoretical considerations and preliminary experimental results. J Sediment Petrol, 35: 339-347
[37]
Spencer R J. 1987. Origin of Ca-Cl brines in devonian formations, Western Canada sedimentary basin. Appl Geochem, 2: 373-384
[38]
Sugitani K, Yamashita F, Nagaoka T, et al. 2006. Geochemistry and sedimentary petrology of Archean clastic sedimentary rocks at Mt.Goldsworthy, Pilbara Craton, Western Australia: Evidence for the early evolution of continental crust and hydrothermal alteration. Precambrian Res, 147: 124-147
[39]
Sun S S, McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. In: Sunders A D, Norry M J. eds. Mamatism in the Ocean Basin. London Geol Soc Spec Publ, 42: 313-345
[40]
Tarasov V G, Gebruk A V, Mironov A N, et al. 2005. Deep-sea and shallow-water hydrothermal vent communities: Two different phenomena. Chem Geol, 224: 5-39
[41]
Taylor R, Mclenan S M. 1985. The continental crust: Its composition and evolution. London: Blackwell. 57-72
[42]
Tribovillard N, Algeo T J, Lyons T, et al. 2006. Trace metals as paleoredox and paleoproductivity proxies: An update. Chem Geol, 232: 12-32
[43]
Tritlla J, Cardellach E. 2001. Origin of vein hydrothermal carbonates in triassic limestones of the Espadan Ranges Iberian Chain, E Spain. Chem Geol, 172: 291-305
[44]
Veizer J, Ala D, Azmy K B, et al. 1999. 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater. Chem Geol, 161: 59-88
[45]
Wright D T. 1999. The role of sulphate reducing bacteria and cyanobacteria in dolomite formation in distal ephemeral lakes of the Coorong region, South Australia. Sediment Geol, 126: 147-157
[46]
Wright W R, Johnson A W, Sheltonb K L, et a1. 2000. Fluid migration and rock interactions during dolomitisation of the Dinantian Irish Midlands and Dublin Basin. J Geochem Explor, 69-70: 159-164
Al-Aasm I S. 2003. Origin and characterization of hydrothermal dolomite in the Western Canada Sedimentary basin. J Geochem Explor, 78-79: 9-15
[62]
Al-Aasm I S, Vernon M. 2007. Waulsortian-like mounds of the Mississippian Pekisko formation, Northwestern Alberta: Petrographic and chemical attributes. Mar Petr Geol, 24: 616-631
[63]
Blendinger W. 2004, Sea level changes versus hydrothermal diagenesis: Origin of Triassic carbonate platform cycles in the dolomites, Italy. Sediment Geol, 169: 21-28
[64]
Boni M, Iannacea A, Bechstadtb T, et al. 2000. Hydrothermal dolomites in SW Sardinia (Italy) and Cantabria (NW Spain): Evidence for late to post-Variscan widespread Fluid-flow Events. J Geochem Explor, 69-70: 225-228
[65]
Bonnemaison M. 1986. Les “filons de quartz aurifère”: Un casparticulier de shear zone aurifère. Chron Rech Minière, 54: 55-66
[66]
Brigaud B, Durlet C, Deconinck J, et al. 2009. The origin and timing of multiphase cementation in carbonates: Impact of regional scale geodynamic events on the Middle Jurassic Limestones Diagenesis (Paris Basin, France). Sediment Geol, 222: 161-180
[67]
Brown A C. 1993. Sediment-host of stratiform copper deposits. Geosci Can, 19: 125-141
[68]
Caline B, Sudrie M, López-Horgue M A, et al. 2006. Fault-related hydrothermal dolomites of cretaceous platform carbonates outcropping in the Karrantza area (North Spain): Lessons learned for a better characterisation of subsurface dolomite reservoirs. In: 17th International Sedimentological Congress, Fukuoka, Japan
[69]
Do Campo M, del P C, Jiménez-Millán J, et al. 2007. Clay mineral assemblages and analcime formation in a Palaeogene fluvial-lacustrine sequence (Maíz Gordo Formation Palaeogen) from northwestern Argentina. Sediment Geol, 201: 56-74
[70]
Chen D Z, Qing H R, Yang C. 2004. Multistage hydrothermal dolomites in the Middle Devonian(Givetian) carbonates from Guilin area, South China. Sedimentary, 561: 1029-1051
[71]
Davies G R, Smith Jr L B. 2006. Structurally controlled hydrothermal dolomite reservoir facies: An overview. AAPG Bull, 90: 1641-1690
[72]
Deckker P D, Last W M. 1988. Modern dolomite deposition in continental, Saline Lakes, Western Victoria, Australia. Geology, 16: 29-32
[73]
Dehler C M, Elrick M, Bloch J D, et al. 2005. High-resolution δ13C Stratigraphy of Chuar Group (ca 770-742Ma) Grand Canyon: Implications for Mid- Neoproterozoic climate change. Geol Soci Am Bull, 117: 32-45
[74]
Faure G. 1986. Principles of Isotope Geology. 2nd ed. New York: John Wiley and Sons. 160-230
[75]
Folk R L, Land L S. 1975. Mg/Ca ratio and salinity; two controls over crystallization of dolomite. AAPG Bull, 59: 60-68
[76]
Folk R L. 1993. SEM imaging of bacteria and nannobacteria in carbonate sediments and rocks. J Sediment Petrol, 63: 990-999
[77]
Frimmel H E. 2009. Trace element distribution in Neoproterzoic carbonates as palaeoenvironmental indicator. Chem Geol, 258: 338-353
[78]
Gasparrinia M, Bechstadta T, Bonib M. 2006. Massive Hydrothermal Dolomites in the Southwestern Cantabrian Zone (Spain) and their relation to the Late Variscan evolution. Mar Petrol Geol, 23: 543-568
[79]
Ghobarkar H, Sch？f O. 1990. Effect of temperature on hydrothermal synthesis of analcime and Visite. Mat Sci Eng, B60: 163-167
[80]
Humphrisi S E, Bach W. 2005. On the Sr isotope and REE compositions of anhydrites from the TAG seafloor hydrothermal system. Geochim Cosmochim Acta, 69: 1511-1525
[81]
Kimura H, Watanabe Y. 2001. Ocean anoxia at the Precambrian-Cambrian boundary. Geology, 29: 995-998
[82]
Klinkhammer G P, Elderfield H, Edmond J M, et al. 1994. Geochemical implications of rare Earth element patterns in hydrothermal fluids from Mid-ocean ridges. Geochim Cosmochim Acta, 58: 5105-5113
[83]
Lavoie D, Chi G, Alpert B P, et al. 2005. Hydrothermal dolomitization in the lower Ordovician romaine formation of the Anticosti Basin: Significance for hydrocarbon exploration. B Can Petrol Geol, 53: 454-471
