Role of structural inheritance in the gravitational deformation of the Monviso meta-ophiolite Complex: the Pui-Orgiera serpentinite landslide (Varaita Valley, Western Alps)
Depending on its chemical and mineralogical composition, the serpentinite represents a peculiar rocky material, which plays a significant role in influencing pedogenetic weathering, vegetation ecology, geo-mechanical and tectonic processes, as well as gravitational slope failure. In serpentinite-bea...
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Published in | Journal of maps Vol. 15; no. 2; pp. 372 - 381 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Abingdon
Taylor & Francis
03.07.2019
Taylor & Francis Ltd Taylor & Francis Group |
Subjects | |
Online Access | Get full text |
ISSN | 1744-5647 1744-5647 |
DOI | 10.1080/17445647.2019.1602854 |
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Abstract | Depending on its chemical and mineralogical composition, the serpentinite represents a peculiar rocky material, which plays a significant role in influencing pedogenetic weathering, vegetation ecology, geo-mechanical and tectonic processes, as well as gravitational slope failure. In serpentinite-bearing environments the response to gravitational stress is more effective than in other rock types. In the Monviso meta-ophiolite Complex (Western Alps), a close relation between landsliding and serpentinite rock occurrences is particularly evident. Our geological map (
Main Map
), at a scale 1:10,000, illustrates the geology and geomorphological features of the Pui-Orgiera giant (2.98 km
2
) complex landslide, located on the southern slope of the Monviso Massif. This map clearly documents that the characteristics and kinematics of the landslide are closely associated to the anomalous thickening and widening increase of the Baracun Shear Zone, a remnants of an intra-oceanic detachment fault which separates serpentinite and meta-intrusives from metabasalt and metasediments of the Monviso meta-ophiolite Complex. |
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AbstractList | Depending on its chemical and mineralogical composition, the serpentinite represents a peculiar rocky material, which plays a significant role in influencing pedogenetic weathering, vegetation ecology, geo-mechanical and tectonic processes, as well as gravitational slope failure. In serpentinite-bearing environments the response to gravitational stress is more effective than in other rock types. In the Monviso meta-ophiolite Complex (Western Alps), a close relation between landsliding and serpentinite rock occurrences is particularly evident. Our geological map (
Main Map
), at a scale 1:10,000, illustrates the geology and geomorphological features of the Pui-Orgiera giant (2.98 km
2
) complex landslide, located on the southern slope of the Monviso Massif. This map clearly documents that the characteristics and kinematics of the landslide are closely associated to the anomalous thickening and widening increase of the Baracun Shear Zone, a remnants of an intra-oceanic detachment fault which separates serpentinite and meta-intrusives from metabasalt and metasediments of the Monviso meta-ophiolite Complex. Depending on its chemical and mineralogical composition, the serpentinite represents a peculiar rocky material, which plays a significant role in influencing pedogenetic weathering, vegetation ecology, geo-mechanical and tectonic processes, as well as gravitational slope failure. In serpentinite-bearing environments the response to gravitational stress is more effective than in other rock types. In the Monviso meta-ophiolite Complex (Western Alps), a close relation between landsliding and serpentinite rock occurrences is particularly evident. Our geological map (Main Map), at a scale 1:10,000, illustrates the geology and geomorphological features of the Pui-Orgiera giant (2.98 km2) complex landslide, located on the southern slope of the Monviso Massif. This map clearly documents that the characteristics and kinematics of the landslide are closely associated to the anomalous thickening and widening increase of the Baracun Shear Zone, a remnants of an intra-oceanic detachment fault which separates serpentinite and meta-intrusives from metabasalt and metasediments of the Monviso meta-ophiolite Complex. |
Author | Fioraso, Gianfranco Festa, Andrea Balestro, Gianni Lanteri, Luca |
Author_xml | – sequence: 1 givenname: Gianfranco surname: Fioraso fullname: Fioraso, Gianfranco email: gianfranco.fioraso@cnr.it organization: Institute of Geoscience and Earth Resources - National Research Council – sequence: 2 givenname: Gianni surname: Balestro fullname: Balestro, Gianni organization: Department of Earth Sciences, University of Torino – sequence: 3 givenname: Andrea surname: Festa fullname: Festa, Andrea organization: Department of Earth Sciences, University of Torino – sequence: 4 givenname: Luca surname: Lanteri fullname: Lanteri, Luca organization: ARPA Piemonte - Regional Agency for the Protection of the Environment |
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CitedBy_id | crossref_primary_10_1080_17445647_2019_1698473 crossref_primary_10_3390_plants13162280 crossref_primary_10_1080_17445647_2020_1784806 crossref_primary_10_1080_17445647_2020_1824825 crossref_primary_10_3390_min11040411 crossref_primary_10_1080_17445647_2020_1854130 |
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SubjectTerms | Chemical composition Ecological effects Geologic mapping Geological mapping Geology Geomorphology Gravitation Gravity Heredity Kinematics landslide Landslides Landslides & mudslides Massifs Monviso meta-ophiolite Complex rock flow Rocks serpentinite Shear zone talcschist Tectonics Thickening |
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Title | Role of structural inheritance in the gravitational deformation of the Monviso meta-ophiolite Complex: the Pui-Orgiera serpentinite landslide (Varaita Valley, Western Alps) |
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