The Vembo Shales (Republic of the Congo): new insights on the transition from lacustrine to marine settings in the South Atlantic

التفاصيل البيبلوغرافية
العنوان: The Vembo Shales (Republic of the Congo): new insights on the transition from lacustrine to marine settings in the South Atlantic
المؤلفون: Delhaye-Prat, Vincent, Dupont, G., Buratti, N., Moron, J.M., Esnault, J., Perrichot, Vincent, Al., Et
المساهمون: Géosciences Rennes (GR), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)
المصدر: 35th International Geological Congress
https://insu.hal.science/insu-01450905
35th International Geological Congress, Aug 2016, Le Cap, South Africa. Paper n°2850
بيانات النشر: HAL CCSD
سنة النشر: 2016
المجموعة: Archive Ouverte de l'Université Rennes (HAL)
مصطلحات موضوعية: [SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology, [SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy
جغرافية الموضوع: Le Cap, South Africa
الوصف: International audience ; The Vembo Shales, originally defined in Gabon, are also recorded in Congo where they are recognized as the “terme argilo-carbonaté”[1]. This member of the Chéla Formation (Aptian), deposited just below the evaporites of the Loémé Formation, was recently identified in outcrops located 70 km to the NE of Pointe-Noire (Fig. 1) along the National Road 1 (RN1). These outcrops were not stratigraphically well-constrained due to the lack of fauna and were previously attributed [2] to undifferentiated Cretaceous (Fig.1) based on facies characteristics that are similar to succession exposed in outcrops in Gabon.
نوع الوثيقة: conference object
اللغة: English
الاتاحة: https://insu.hal.science/insu-01450905
رقم الانضمام: edsbas.270B0502
قاعدة البيانات: BASE