Cosmic ray exposure dating on the large landslide of Séchilienne (Western Alps): A synthesis to constrain slope evolution

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• 作者：Sté ; phane Schwartz^a ; ^{stephane.schwartz@univ-grenoble-alpes.fr} ; Swann Zerathe^a ; Denis Jongmans^a ; Laurent Baillet^a ; Julien Carcaillet^a ; Laurence Audin^a ; Thierry Dumont^a ; Didier Bourlè ; s^b ; Ré ; gis Braucher^b ; Vincent Lebrouc^a
• 关键词：Western Alps ; Sé ; chilienne landslide ; Cosmic ray exposure dating ; Slope evolution
• 刊名：Geomorphology
• 出版年：2017
• 出版时间：1 February 2017
• 年：2017
• 卷：278
• 期：Complete
• 页码：329-344
• 全文大小：4619 K
• 卷排序：278

文摘

The 60 × 106 m3 Séchilienne landslide (Belledonne Massif, Western Alps) is located on the right bank of the East-West trending Romanche valley which is shaped by glacial and alluvial processes during the Quaternary. Its head scarp (> 35 m high) was dated by Le Roux et al. (2009) using the cosmic ray exposure (CRE) method. Even though these previous results revealed that the initiation of the instability occurred several thousand years after ice down-wastage in the valley, the internal landslide evolution is not constrained. In this paper, we provide 63 additional 10Be samples collected from the internal scarps and the main scarp, as well as on glacially polished rock surfaces. The aim is to constrain the global landslide kinematics (internal and head scarps) and its relationship with glacier retreat. Results from glacially polished surfaces point out that complex shielding processes (relict moraines, soil deposits and seasonal snow cover) might have affected rock dating. Despite scattering of the resulting ages, the dataset shows that the glacial retreat was achieved between 17.5 and 13 ka. Exposure ages obtained on gravitational scarps reveal that the landslide initiation occurred 8 to 6 ka ago. From the initiation until 2 ka the gravitational kinematics was slow (~ 2 mm·year− 1) and focused around the head scarp, leading to a general slope subsidence. After 2 ka, the exposure rates increased significantly (~ 8 mm·year− 1) with the development of pervasive internal deformation of the landslide mass. This new scenario for the Séchilienne slope reflects a progressive rock-slope weakening since 8 ka, associated with a continuous activity of a deep-seated surface failure.