Your browser doesn't support javascript.
loading
The deep origin of ground fissures in the Kenya Rift Valley.
Jia, Zhijie; Wu, Hongjie; Peng, Jianbing; Lu, Quanzhong; Huang, Weiliang; Liu, Chuntao; Wang, Feiyong; Liu, Yang; He, Ming.
Afiliación
  • Jia Z; School of Geological Engineering and Geomatics, Chang'an University, Xi'an, China.
  • Wu H; School of Earth Science and Resources, China University of Geosciences, Beijing, China.
  • Peng J; School of Geological Engineering and Geomatics, Chang'an University, Xi'an, China. dicexy_1@126.com.
  • Lu Q; Key Laboratory of Western China Mineral Resources and Geological Engineering, Xi'an, China. dicexy_1@126.com.
  • Huang W; School of Geological Engineering and Geomatics, Chang'an University, Xi'an, China.
  • Liu C; Key Laboratory of Western China Mineral Resources and Geological Engineering, Xi'an, China.
  • Wang F; School of Geological Engineering and Geomatics, Chang'an University, Xi'an, China.
  • Liu Y; Key Laboratory of Western China Mineral Resources and Geological Engineering, Xi'an, China.
  • He M; School of Earth Science and Resources, China University of Geosciences, Beijing, China.
Sci Rep ; 13(1): 3672, 2023 Mar 04.
Article en En | MEDLINE | ID: mdl-36871127
Intense volcanic and geothermal activities characterize the Great Rift Valley of East Africa. Ground fissure disasters of the Great Rift Valley have garnered increasing attention in recent years. Through field investigations, trenching, geophysical exploration, gas sampling and analysis, we determined the distribution and origin of 22 ground fissures within the Kedong Basin of the Central Kenya Rift. These ground fissures caused varying degrees of damage to roads, culverts, railways, and communities. Trenching and geophysical exploration have shown that ground fissures in sediments are connected to rock fractures with gas escaping. The gases expelled from the rock fractures contained methane and SO2, which were absent in the normal atmosphere, and 3He/4He ratios in gases measured further indicated that the volatiles were derived from the mantle, suggesting that these rock fractures extended deep into the underlying bedrock. Spatial correlations with rock fractures demonstrate the deep origin of these ground fissures, which are associated with active rifting, plate separation, and volcanism. The ground fissures are formed due to movement on the deeper rock fractures, and then the gas escapes through the fissures. Determining the unusual origin of these ground fissures can not only guide infrastructure development and urban planning but also contribute to the safety of local communities.

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Idioma: En Revista: Sci Rep Año: 2023 Tipo del documento: Article País de afiliación: China Pais de publicación: Reino Unido

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Idioma: En Revista: Sci Rep Año: 2023 Tipo del documento: Article País de afiliación: China Pais de publicación: Reino Unido