意大利马拉蒂亚山谷复杂滑坡的运动演化与剪切强度

Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science Pub Date : 2001-01-01 DOI:10.1016/S1464-1917(01)00066-6

G. Toni , V. Rizzo

{"title":"意大利马拉蒂亚山谷复杂滑坡的运动演化与剪切强度","authors":"G. Toni , V. Rizzo","doi":"10.1016/S1464-1917(01)00066-6","DOIUrl":null,"url":null,"abstract":"<div><p>It is suggested that a structural kinematic mechanism could have formed the so-called Maratea “Sackung” (A. GUERRICCHIO, G. MELIDORO, 1979) (more comprehensible as the “Sagging” phenomenon) and enabled the complex surrounding landslides to take place.</p><p>For the same deformation speed, the change in resistance as a function of different stress conditions was identified by means of triaxial testing carried out on test pieces obtained from both undisturbed and remoulded samples of the basal clay complex with “Sicilide” affinity.</p><p>Finally, the results obtained were compared with slide velocity during the last decade and the various thicknesses of the partially detrital mass in which the main landslides occur.</p></div>","PeriodicalId":101026,"journal":{"name":"Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science","volume":"26 9","pages":"Pages 677-681"},"PeriodicalIF":0.0000,"publicationDate":"2001-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1464-1917(01)00066-6","citationCount":"1","resultStr":"{\"title\":\"Kinematic evolution and shear strength in the complex landslides of the Maratea valley (PZ, Italy)\",\"authors\":\"G. Toni , V. Rizzo\",\"doi\":\"10.1016/S1464-1917(01)00066-6\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>It is suggested that a structural kinematic mechanism could have formed the so-called Maratea “Sackung” (A. GUERRICCHIO, G. MELIDORO, 1979) (more comprehensible as the “Sagging” phenomenon) and enabled the complex surrounding landslides to take place.</p><p>For the same deformation speed, the change in resistance as a function of different stress conditions was identified by means of triaxial testing carried out on test pieces obtained from both undisturbed and remoulded samples of the basal clay complex with “Sicilide” affinity.</p><p>Finally, the results obtained were compared with slide velocity during the last decade and the various thicknesses of the partially detrital mass in which the main landslides occur.</p></div>\",\"PeriodicalId\":101026,\"journal\":{\"name\":\"Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science\",\"volume\":\"26 9\",\"pages\":\"Pages 677-681\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2001-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/S1464-1917(01)00066-6\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1464191701000666\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1464191701000666","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}

引用次数: 1

摘要

有人认为，一种结构运动机制可能形成了所谓的马拉蒂亚“凹陷”(a . GUERRICCHIO, G. MELIDORO, 1979)(更容易理解为“凹陷”现象)，并使周围复杂的滑坡发生。在相同的变形速度下，通过对具有“Sicilide”亲和性的基础粘土复合体的未扰动和重塑样品的试件进行三轴试验，确定了阻力随不同应力条件的变化。最后，将所得结果与近十年来的滑动速度和主要滑坡发生的部分碎屑体的不同厚度进行了比较。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

查看原文本刊更多论文

Kinematic evolution and shear strength in the complex landslides of the Maratea valley (PZ, Italy)

It is suggested that a structural kinematic mechanism could have formed the so-called Maratea “Sackung” (A. GUERRICCHIO, G. MELIDORO, 1979) (more comprehensible as the “Sagging” phenomenon) and enabled the complex surrounding landslides to take place.

For the same deformation speed, the change in resistance as a function of different stress conditions was identified by means of triaxial testing carried out on test pieces obtained from both undisturbed and remoulded samples of the basal clay complex with “Sicilide” affinity.

Finally, the results obtained were compared with slide velocity during the last decade and the various thicknesses of the partially detrital mass in which the main landslides occur.

求助全文

通过发布文献求助，成功后即可免费获取论文全文。去求助

来源期刊

Physics and Chemistry of the Earth, Part C: Solar, Terrestrial & Planetary Science

自引率

0.00%

发文量