Conference
The Vembo Shales (Republic of the Congo): new insights on the transition from lacustrine to marine settings in the South Atlantic
العنوان: | The Vembo Shales (Republic of the Congo): new insights on the transition from lacustrine to marine settings in the South Atlantic |
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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 |
الوصف غير متاح. |