Rifting Kinematics Produced by Magmatic and Tectonic Stresses in the North Volcanic Zone of Iceland

In the North Volcanic Zone of Iceland, we studied with the greatest possible detail the complete structural architecture and kinematics of the whole Theistareykir Fissure Swarm (ThFS), an N-S-trending, 70 km long active rift. We made about 7500 measurements along 6124 post-Late Glacial Maximum (LGM)...

Deskribapen osoa

Gorde:
Xehetasun bibliografikoak
Egile Nagusiak: Alessandro Tibaldi, Fabio Luca Bonali, Federico Pasquaré Mariotto, Noemi Corti, Elena Russo, Páll Einarsson, Ásta Rut Hjartardóttir
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: Frontiers Media S.A. 2020-06-01
Saila:Frontiers in Earth Science
Gaiak:
rift
Iceland
fault
fracture
stress
dyke
Sarrera elektronikoa:https://www.frontiersin.org/article/10.3389/feart.2020.00174/full
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