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Volumn 2, Issue , 2008, Pages 135-138

Preliminary palaeontological observations on some examples of "nummulite banks": Sedimentary or biological origin?

Author keywords

Carbonate platforms; Eocene; Foraminiferal assemblages; Hydrodynamic energy; Mediterranean; Nummulite banks; Paleoenvironmental models

Indexed keywords


EID: 79956058245     PISSN: 20358008     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Conference Paper
Times cited : (13)

References (9)
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    • Event-stratification in nummulite accumulations and in shell beds from the Eocene of Egypt
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    • (1982) Cyclic and Event Stratification , pp. 248-262
    • Aigner, T.1
  • 2
    • 0000032728 scopus 로고
    • Facies and origin of nummulitic buildups: An example from the Giza Pyramids Plateau (Middle Eocene, Egypt)
    • AIGNER T. (1983) - Facies and origin of nummulitic buildups: an example from the Giza Pyramids Plateau (Middle Eocene, Egypt). N. Jb. Geol. Paläont. Abh., 166(3), 347-368.
    • (1983) N. Jb. Geol. Paläont. Abh. , vol.166 , Issue.3 , pp. 347-368
    • Aigner, T.1
  • 3
    • 0021851595 scopus 로고
    • Biofabrics as dynamic indicators in nummulite accumulations
    • AIGNER T. (1985) - Biofabrics as dynamic indicators in nummulite accumulations. J. Sedim. Petrol., 55(1), 131-134.
    • (1985) J. Sedim. Petrol. , vol.55 , Issue.1 , pp. 131-134
    • Aigner, T.1
  • 4
    • 0002788641 scopus 로고
    • L'évolution des Nummulitinae en tant que facteur de modification des dépôts littoraux
    • ARNI P. (1965) - L'évolution des Nummulitinae en tant que facteur de modification des dépôts littoraux. Mém. Bur. Rech. Géol. Min., 32, 7-20.
    • (1965) Mém. Bur. Rech. Géol. Min. , vol.32 , pp. 7-20
    • Arni, P.1
  • 5
    • 0007341168 scopus 로고
    • Considérations paléoécologiques et interprétation des calcaires de l'Eocène du Véronais
    • ARNI P. & LANTERNO E. (1972) - Considérations paléoécologiques et interprétation des calcaires de l'Eocène du Véronais. Arch. Sci., 25(2), 251-283.
    • (1972) Arch. Sci. , vol.25 , Issue.2 , pp. 251-283
    • Arni, P.1    Lanterno, E.2
  • 6
    • 20644467488 scopus 로고    scopus 로고
    • Sediment production and dispersal on foraminifera-dominated early Tertiary ramps: The Eocene El Garia Formation, Tunisia
    • DOI 10.1111/j.1365-3091.2005.00709.x
    • BEAVINGTON-PENNEY S. J., WRIGHT W. P. & RACEY A. (2005) - Sediment production and dispersal on foraminiferadominated early Tertiary ramps: the Eocene El Garia Formation, Tunisia. Sedimentology, 52, 537-569. (Pubitemid 40836603)
    • (2005) Sedimentology , vol.52 , Issue.3 , pp. 537-569
    • Beavington-Penney, S.J.1    Wright, V.P.2    Racey, A.3
  • 7
    • 0005679050 scopus 로고
    • Les "bancs à Nummulites" de l'Eocène mésogéen et leurs implications
    • DECROUEZ D. & LANTERNO E. (1979) - Les "bancs à Nummulites" de l'Eocène mésogéen et leurs implications. Arch. Sci., 32(1), 67-94.
    • (1979) Arch. Sci. , vol.32 , Issue.1 , pp. 67-94
    • Decrouez, D.1    Lanterno, E.2
  • 8
    • 0034650871 scopus 로고    scopus 로고
    • Recognition of stratigraphic sequences in carbonate platform and slope deposits: Empirical models based on microfacies analysis of Palaeogene deposits in southeastern Spain
    • DOI 10.1016/S0031-0182(99)00117-0, PII S0031018299001170
    • GEEL T. (2000) - Recognition of stratigraphic sequences in carbonate platform and slope deposits: empirical models based on microfacies analysis of Palaeogene deposits in southeastern Spain. Palaeogeogr., Palaeoclimatol., Palaeoecol., 155(3-4), 211-238. (Pubitemid 30061510)
    • (2000) Palaeogeography, Palaeoclimatology, Palaeoecology , vol.155 , Issue.3-4 , pp. 211-238
    • Geel, T.1
  • 9
    • 33645984543 scopus 로고    scopus 로고
    • Hydrodynamic behaviour of Nummulites: Implications for depositional models
    • JORRY S. J., HASLER C.-A. & DAVAUD E. (2006) - Hydrodynamic behaviour of Nummulites: implications for depositional models. Facies, 52, 221-235.
    • (2006) Facies , vol.52 , pp. 221-235
    • Jorry, S.J.1    Hasler, C.-A.2    Davaud, E.3


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.