Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Francho Gracia Puzo"'
The southern Pyrenean Zone shows a classical thin-skinned fold-and-thrust belt. Particularly interesting is the thrust sequence detached in the Upper Triassic low-strength level cropping out in the central-western sector of the chain (Leyre-Orba thru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5d4a7e2bbc2991fc00a9bf22e34add30
https://doi.org/10.5194/egusphere-egu22-5905
https://doi.org/10.5194/egusphere-egu22-5905
With the objective of mapping strain on the footwall of a thrust in an orogenic context (Leyre thrust, South Pyrenean Range), more than 1500 unoriented shale fragments (0.7-6.2 g) have been collected. Scalar data (degree of anisotropy P and shape par
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a57fa65a5f742d3704e513d7828c17f
https://doi.org/10.5194/egusphere-egu21-6377
https://doi.org/10.5194/egusphere-egu21-6377
With the objective of mapping strain around a thrust front in an orogenic context (Pyrenean Range), 757 shale fragments (0.7-6.2 g) have been collected in 49 sites. Scalar data (degree of anisotropy P and shape parameter T), together with ellipse of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d40f098886eba919f7d169fd8c95e247
https://doi.org/10.5194/egusphere-egu2020-11399
https://doi.org/10.5194/egusphere-egu2020-11399