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1. Analyse géotechnique et évaluation du risque lié à l’instabilité le long de la falaise du quartier Hassan (Rabat-Maroc) Geotechnical analysis and evaluation of the instability risk along the Hassan district cliff (Rabat-Morocco)

3. The Atlas System

6. FRIPON: a worldwide network to track incoming meteoroids

8. FRIPON: a worldwide network to track incoming meteoroids

11. Palaeomagnetism of the upper volcanic supergroup, southern part of the Sierra Occidental, Mexico

12. Synthèses et tablaux de corrélations

13. The Atlas System

15. Chronology of the Eocene continental deposits of Africa: Magnetostratigraphy and biostratigraphy of the El Kohol and Glib Zegdou Formations, Algeria

29. FRIPON: a worldwide network to track incoming meteoroids

30. FRIPON: a worldwide network to track incoming meteoroids

31. A new primate community from the earliest Oligocene of the Atlantic margin of Northwest Africa: Systematic, paleobiogeographic, and paleoenvironmental implications.

32. A new small pliopithecoid primate from the Middle Miocene of Thailand.

33. Integrated Paleoenvironmental Reconstruction and Taphonomy of a Unique Upper Cretaceous Vertebrate-Bearing Locality (Velaux, Southeastern France).

34. First hominoid from the Late Miocene of the Irrawaddy Formation (Myanmar).

35. Late middle Eocene epoch of Libya yields earliest known radiation of African anthropoids.

36. Gaudeamus lavocati sp. nov. (Rodentia, Hystricognathi) from the early Oligocene of Zallah, Libya: first African caviomorph?

37. Amber from western Amazonia reveals Neotropical diversity during the middle Miocene.

38. New remains of the enigmatic cetartiodactyl Bugtitherium grandincisivum Pilgrim, 1908, from the upper Oligocene of the Bugti Hills (Balochistan, Pakistan).

39. Anthropoid primates from the Oligocene of Pakistan (Bugti Hills): data on early anthropoid evolution and biogeography.

40. A Middle Miocene hominoid from Thailand and orangutan origins.

41. A fossil lemur from the Oligocene of Pakistan.

42. A lower jaw of Pondaungia cotteri from the Late Middle Eocene Pondaung Formation (Myanmar) confirms its anthropoid status.

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