Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Eric James Ryan"'
Autor:
Bjørn Eske Sørensen, Eric James Ryan, Rune Larsen, Stefanie Lode, Jostein Røstad, Thomas B. Grant
Planar deformation features are a common feature in shock-deformed olivine, both experimentally in conditions corresponding to crustal shear zones [1] and impact structures e.g., [2] and in deep crustal shear zones [3, 4]. Hence, the identification o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::18610db82793e6e4e441c9cb69d54b9d
https://doi.org/10.5194/egusphere-egu23-13208
https://doi.org/10.5194/egusphere-egu23-13208
Autor:
Eric James Ryan, Paolo S. Garofalo, Giulio Viola, Giovanni Musumeci, Samuele Papeschi, Francesco Mazzarini
Publikováno v:
Journal of Maps, Vol 17, Iss 2, Pp 533-546 (2021)
Journal of Maps
Journal of Maps
We document the tectonic and metamorphic evolution of thrust nappes of the eastern island of Elba. The area exposes a natural cross section of the Northern Apennines hinterland, from the metamorphic basement units to the overlying continent- and ocea
We provide here in situ evidence from a network of well-preserved extensional shear zones cutting a rift related lower crustal Reinfjord Ultramafic Complex, Seiland Igneous Province, that formed in the late Ediacaran. Our results can explain seismic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5dec798d683204d17b68690bbaecbbea
https://doi.org/10.5194/egusphere-egu22-10545
https://doi.org/10.5194/egusphere-egu22-10545
The permeability structure of a fault zone is strongly dependent on the occurrence of meso-scale fracture patterns within the damage zone. Here, structural analyses of Virtual Outcrop Models (VOM) integrated with Discrete Fracture Network (DFN) model
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ccf29113091496666ead22801f4d534b
https://hdl.handle.net/11585/831393
https://hdl.handle.net/11585/831393
Autor:
Giovanni Musumeci, Bjørn Eske Sørensen, Giulio Viola, Francesco Mazzarini, Espen Torgersen, Morgan Ganerød, Eric James Ryan, Samuele Papeschi
The E-vergent Northern Apennines formed by Oligocene-Miocene convergence and westward subduction of Adria beneath Europe. Extension ensued in the Mid-Late Miocene reflecting lower plate roll-back and causing opening of the back-arc Northern Tyrrhenia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6c40e664cd8a814d3c90f98c58f73417
https://hdl.handle.net/11585/819860
https://hdl.handle.net/11585/819860
The detailed characterization of internal fault zone architecture and petrophysical and geomechanical properties of fault rocks is fundamental to understanding the flow and mechanical behaviour of mature fault zones. The Goddo normal fault (Bømlo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7931a42135d493d1e5806ba8485926e7
https://doi.org/10.5194/egusphere-egu2020-6691
https://doi.org/10.5194/egusphere-egu2020-6691
Autor:
Eric James Ryan, Alf Andre Orvik, Bjørn Eske Sørensen, Thomas B. Grant, Rune B. Larsen, Jørgen Sakariasen
The coupling of CO2 emissions and tectonic activity in active plate margins is becoming increasingly prominent, as remote sensing techniques make this relationship readily observable on a global sc...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f33d700e03142df042f1dc171ebbf48b
https://doi.org/10.1002/essoar.10502275.1
https://doi.org/10.1002/essoar.10502275.1
Autor:
Giulio Viola, Hans-Joachim Massonne, Francesco Mazzarini, Samuele Papeschi, Giovanni Musumeci, Eric James Ryan
The Acquadolce Subunit on the Island of Elba, Italy, records blueschist facies met- amorphism related to the Oligocene–early Miocene stages of continental collision in the Northern Apennines. The blueschist facies metamorphism is represented by gla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cbc8c36f511f11c4247a897f7074d585
https://hdl.handle.net/11585/759134
https://hdl.handle.net/11585/759134
Publikováno v:
Earth and Planetary Science Letters
This study aims to understand the process behind the worldwide connection between deep crustal/upper mantle earthquakes and CO2 emissions along faults in rift zones. We do this by studying CO2-induced mineral reactions that facilitate strain localiza
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f2a44f52035e64330df98c081b338688
https://hdl.handle.net/11250/2627225
https://hdl.handle.net/11250/2627225