Carr D L, Scott A J. 1990. Late Pennsylvanian storm-dominated shelf sand ridges,Sacramento Mountains,New Mexico[J]. Journal of Sedimentary Petrology,60(4):592-607.
[13]
Colombie C,Schnyder S,Carcel. 2012. Shallow-water marl-limestone alternations in the Late Jurassic of western France:Cycles,storm event deposits or both[J]. Sedimentary Geology,271-272:28-43.
[14]
Dalziel I W D. 1997. Neoproterozoic-Paleozoic geography and tectonics:Review,hypothesis,environmental speculation[J]. GSA Bullet,109(1):16-42.
[15]
Dattilo B F,Brett C E,Tsujita C J,et al. 2008. Sediment supply versus storm winnowing in the development of muddy and shelly interbeds from the Upper Ordovician of the Cincinnati region,USA[J]. Canada Journal of Earth Science,45(2):243-265.
[16]
Dezileau L,Sabatier P,Blanchemanche P,et al. 2011. Intense storm activity during the Little Ice Age on the French Mediterranean coast[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,299(1-2):289-297.
[17]
Ding Y,Bai Z,Liu J, et al. 2008. Multiple origins for flat-pebble limestones and sedimentary environments of the Upper Cambrian Gushan Formation at Tangwangzhai in Shandong Province[J]. Journal of Palaeogeography,4(2):125-138.
[18]
Donnelly J P,Woodruff J D. 2007. Intense hurricane activity over the past 5000 years controlled by El Nino and the West African monsoon[J]. Nature,447(10):465-468.
[19]
Eolf J D. 2014. Sedimentary facies of the upper Cambrian(Furongian;Jiangshanian and Sunwaptan)Tunnel City Group,Upper Mississippi Valley:Newinsight on the old stormy debate[J]. Sedimentary Geology,302(1):102-121.
[20]
Flügel E. 2009. Microfacies of Carbonate Rocks[M]. Springer Verlag,Berlin,724-738.
[21]
Garrison J R,Miller S P,Mestas-nunez A, et al. 2013. Record of historical gulf of mexico storms preserved in the stratigraphy of gum hollow delta,Nueces Bay,Texas,U.S.A.: An example of tropical-cyclone-induced hyperpycnal deposition[J]. Journal of Sedimentary Research,83(10):1-11.
[22]
Goff J A,Allison M A,Gulick P S. 2008. Offshore transport of sediment during cyclonic storms:Hurricane Ike(2008),Texas Gulf Coast,USA[J]. Geological Society of America,38(4):351-354.
[23]
Hippensteel S P,Eastin M D,Garcia W J. 2013. The geological legacy of Hurricane Irene:Implications for the fidelity of the paleo-storm record[J]. GSA Today,23(12):4-10.
[24]
Kazmierczak J,Goldring R. 1978. Subtidal flat-pebble conglomerate from the Upper Devonian of Poland:A multiprovenant high-energy product[J]. Geology Magazine,155(5):359-366.
[25]
Kelling G, Mullin P R. 1975. Graded limestones and limestone quartzite couplets: Possible storm-deposits from the Moroccan carboniferous[J]. Sedimentary Geology, 13(3):161-190.
[26]
Kwon Y K,Chough S K,Choi D K, et al. 2002. Origin of limestone conglomerates in the Choson Supergroup(Cambro-Ordovician),mid-east Korea[J]. Sedimentary Geology,146(3-4):265-283.
[27]
Li X,Droser M L. 1999. Lower and Middle Ordovician shell beds from the basin and range province of the Western United States(California,Nevada,and Utah)[J]. Palaios,14(3):215-233.
[28]
Long D G F. 2007. Tempestite frequency curves:A key to Late Ordovician and Early Silurian subsidence,sea-level change,and orbital forcing in the Anticosti foreland basin,Quebec,Canada[J]. Canadian Journal of Earth Science,44(3):413-431.
[29]
Masselink G,Van Heteren S. 2014. Response of wave-dominated and mixed-energy barriers to storms[J]. Marine Geology,352(1):321-347.
[30]
McFarland S. 1999. Allogenic versus autogenic processes in the genesis of Middle Ordovician brachiopod-rich shell beds,Verulam Formation,Ontario[J]. Palaios,14(3):282-287.
[31]
Mohseni H,Al-Aasm I S. 2004. Tempestite deposits on a storm-influenced carbonate ramp:An example from the Pabdeh Formation(Paleogene),Zagros Basin,SW Iran[J]. Journal of Petroleum Geology,27(2):163-178.
[32]
Mount J F,Kidder D. 1993. Combined flow origin of edgewise peloidal conglomerates:Sellick Hill Formation(Lower Cambrian),South Australia[J]. Sedimentology,40(2):315-329.
[33]
Myrow P M. 1992. Bypass-zone tempestite facies model and proximality trends for an anancient muddy shoreline and shelf[J]. Journal of Sedimentray Petrology,62(1):99-115.
[34]
Myrow P M,Hiscott R N. 1991. Shallow-water gravity-flow deposits,Chapel Island Formation,southeast Newfoundland,Canada[J]. Sedimentology,38(5):935-959.
[35]
Myrow P M,Southard J B. 1996. Tempestite deposition[J]. Journal of Sedimentary Research,66(5):875-887.
[36]
Myrow P M,Tice L,Archuleta B, et al. 2004. Flat-pebble conglomerate:Its multiple origins and relationship to metre-scale depositional cycles[J]. Sedimentology,51(5):973-996.
[37]
Myrow P M,Lukens C,Lamb M P, et al. 2008. Dynamics of a transgressive prodeltaic system:Implications for geography and climate within a Pennsylvanian intracratonic basin,Colorado,U.S.A.[J]. Journal of Sedimentar Research,78(8):512-528.
[38]
Perea-lopez A,Perez-valera F. 2012. Tempestite facies models for the epicontinental Triassic carbonates of the Betic Cordillera(southern Spain)[J]. Sedimentology,59(2):646-678.
[39]
Plint A G,Macquaker J H S. 2012. Bed load transport of mud across a wide,storm-influenced ramp:Cenomanian-Turonian Kaskapau Formation,Western Canada foreland basin-reply[J]. Journal of Sedimentary Research,83(11):1200-1201.
[40]
Sabatier P,Dezileau L,Condomines M, et al. 2008. Reconstruction of paleostorm events in a coastal lagoon(Hérault,South of France)[J]. Marine Geology,251(3-4):224-232.
[41]
Savrda C,Counts J W,Bigham E,et al. 2010. Ichnology of siliceous facies in the Eocene Tallahatta Formation(Eastern United States gulf coastal plain:Implications for depositional conditions,storm processes,and diagenesis[J]. Palaios,25(10):642-655.
[42]
Tamura T,Masuda F. 2005. Bed thickness characteristics of inner-shelf storm deposits associated with a transgressive to regressive Holocene wave-dominated shelf,Sendai coastal plain,Japan[J]. Sedimentology,52(6):1375-1396.
[43]
Tsujita C J,Brett C E,Toper M, et al. 2006. Evidence of high-frequency storm disturbance in the Middle Devonian Arkona shale,Southwestern Ontario[J]. Journal of Taphonomy,4(2):49-68.
[44]
Veizer J,Ala D,Azmy K, et al. 1999. 87Sr/86Sr,δ13C and δ18O evolution of Phanerozoic seawater[J]. Chemical Geology,161(1-3):59-88.
[45]
Wanless H R,Tedesco L P,Tyrrell K M. 1987. Production of subtidal tubular and surficial tempestites by Hurricane Kate,Calcos Platform,British West Indies[J]. Journal of Sedimentary Petrology,58(4):739-750.张西娟
Aigner T. 1979. Schill-tempestite in oberen muschelkalk (Trias, sw-Deutschland)[J]. Neues Jahrbuch für Geologie und Palontologie, Abhandlungen, 157:326-343.
[59]
Aigner T. 1985. Storm Depositional Systems[M]. Lecture Notes in Earth Sciences. Springer Verlag,Berlin,174.
[60]
Boyer D L,Droser M I. 2003. Shell beds of the Kanosh and Lehman Formations of Western Utah:Paleoecological and paleoenvironmental interpretations[J]. BYU Geology Studies,47(1):1-15.
[61]
Brandt D S,Elias R J. 1989. Temporal variations in tempestite thickness may be a geologic record of atmospheric CO2[J]. Geology,17(10):951-952.
[62]
Carozzi A V,Gerber M S. 1978. Synsedimentary chert Breccia:A Mississippian tempestite[J]. Journal of Sedimentary Petrology,48(3):705-708.
