2015
DOI: 10.1016/j.sedgeo.2014.10.013
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Calciturbidites and calcidebrites: Sea-level variations or tectonic processes?

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Cited by 41 publications
(65 citation statements)
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“…The facies classification used textural characteristics (Dunham, ; Embry & Klovan, ), constituents (Flügel, ), bed thickness (Table ; McKee & Weir, ), grain sizes (Table ; Blair & McPherson, ), grain sorting (Pettijohn et al ., ) and sedimentary structures (Cook & Mullins, ; Prior et al ., ). A genetic interpretation of the deposits was based on earlier studies focusing on similar carbonate depositional environments (Krause & Oldershaw, ; Mullins & Cook, ; Spence & Tucker, ; Hughes, ; Reijmer et al ., 2015b; Le Goff et al ., , ) and transport processes for MTDs and calciturbidites (Mulder & Alexander, ; Moscardelli & Wood, ).…”
Section: Methodsmentioning
confidence: 99%
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“…The facies classification used textural characteristics (Dunham, ; Embry & Klovan, ), constituents (Flügel, ), bed thickness (Table ; McKee & Weir, ), grain sizes (Table ; Blair & McPherson, ), grain sorting (Pettijohn et al ., ) and sedimentary structures (Cook & Mullins, ; Prior et al ., ). A genetic interpretation of the deposits was based on earlier studies focusing on similar carbonate depositional environments (Krause & Oldershaw, ; Mullins & Cook, ; Spence & Tucker, ; Hughes, ; Reijmer et al ., 2015b; Le Goff et al ., , ) and transport processes for MTDs and calciturbidites (Mulder & Alexander, ; Moscardelli & Wood, ).…”
Section: Methodsmentioning
confidence: 99%
“…A series of studies addressed the key role played by mass transport deposits (MTDs) in governing the slope architecture of both modern (Playton et al ., , and references therein; Mulder et al ., ) and ancient carbonate slope systems (Crevello & Schlager, ; Spence & Tucker, ; Hairabian et al ., ; Reijmer et al ., ,b; Playton & Kerans, ) as well as providing information on the source area (Mullins et al ., , ; Mullins & Hine, ; Ross et al ., ; Borgomano, ; Posamentier & Kolla, ). The terminology of MTDs remains ambiguous due to the disparate definitions and its variable usage (Cook & Mullins, ; Mulder & Cochonat, ; Artoni et al ., ; Meckel, ).…”
Section: Introductionmentioning
confidence: 99%
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“…This "classical" type of highstand shedding has also been documented in a number of other localities around the globe. Evidence for highstand shedding in carbonates elsewhere has taken the form of either: (a) changes in the frequency, thickness or changes in lithology of turbidite deposition in adjacent basins (Bernet, Eberli, & Gilli, 2000;Betzler, Pfeiffer, & Saxena, 2000;Haak & Schlager, 1989;Reijmer & Andresen, 2007;Reijmer, Palmieri, Groen, & Floquet, 2015;Reijmer et al, 2012), (b) differing sediment composition of highstand versus lowstand deposits (Grammer & Ginsburg, 1992), or (c) fine-grained aragonite export during highstand (Paul et al, 2012). Highstand shedding of fine-grained carbonate mud, as seen here, has been observed in numerous other localities (Figure 9 and references therein), with most records substantially shorter than the one reported here.…”
Section: Comparison With Highstand Shedding Elsewherementioning
confidence: 99%
“…During the mid-Cretaceous (Albian-Lower Cenomanian), the formation of the Durance high [Gignoux, 1925;Masse and Philip, 1976] resulted in the subaerial exposure of the Provence area and the development of a major regional unconformity. During the Cenomanian to the Santonian, a rather shallow (~200 m water-depth), east-west trending, narrow and elongated basin was formed (South Provence basin) in a transtensive regime that prevailed mainly during the Turonian-Coniacian [Floquet and Hennuy, 2003;Floquet et al, 2005Floquet et al, , 2006Reijmer et al, 2015]. The South Provence basin was bordered to the north by an extensive carbonate platform and to the south by an emerged crystalline massif [Philip, 1970;.…”
Section: Geodynamic History Of Provencementioning
confidence: 99%