Zobrazeno 1 - 6
of 6
pro vyhledávání: '"C. J. Tulley"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 3, Pp n/a-n/a (2024)
Abstract The Malawi Rift is localized within Precambrian amphibolite‐granulite facies metamorphic belts, bounded by up to 150 km long border faults, and generates earthquakes throughout ∼40 km thick crust. Rift‐related faults are inferred to ex
Externí odkaz:
https://doaj.org/article/254c3dbf444c4212b241e10e60b966a7
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 9, Pp n/a-n/a (2022)
Abstract Geophysical observations indicate that patches of localized fracturing occur within otherwise viscous regions of subduction plate boundaries. These observations place uncertainty on the possible down‐dip extent of the seismogenic zone, and
Externí odkaz:
https://doaj.org/article/b038da036eeb49d8aaf34a7efe33ae5a
Publikováno v:
Geophysical Research Letters. 49
Antigorite serpentinite is expected to occur in parts of subduction plate boundaries, and may suppress earthquake slip, but the dominant deformation mechanisms and resultant rheology of antigorite are unclear. An exhumed plate boundary shear zone exp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b76bbcd228d0181696473c24168da648
https://doi.org/10.1029/2022gl098945
https://doi.org/10.1029/2022gl098945
Autor:
Chris Harris, J. Elis Hoffmann, Petrus le Roux, Matthew S. Tarling, Sophie Scherzer, C. J. Tulley, James M. Scott, Steven A.F. Smith
Publikováno v:
Earth and Planetary Science Letters. 522:198-209
Fluid flow along crustal plate boundary-scale serpentinite shear zones may provide insights into element transfer at one of Earth's most important but least accessible lithological boundaries: the slab-mantle wedge plate interface. For ∼55 km in th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27fa0c9372b510eade7279cb805c4e5b
https://doi.org/10.1016/j.epsl.2019.06.034
https://doi.org/10.1016/j.epsl.2019.06.034
Autor:
C. J. Tulley, Haruna Masuyama, Naoki Nishiyama, Norio Shigematsu, Kazuya Noro, Kohtaro Ujiie, Ake Fagereng
Aseismic megathrust slip down-dip of the seismogenic zone is accommodated by either steady creep or episodic slow slip events (SSEs). However, the geological conditions defining the rheology of megathrust slip remain elusive. Here, we show that subdu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cec8d561505ab3a0ca9cdbdde3c3e66a
https://doi.org/10.5194/egusphere-egu21-1885
https://doi.org/10.5194/egusphere-egu21-1885
Publikováno v:
Science Advances
Hydration allows subducting oceanic crust to be far weaker than previously recognized.
The rheology of the metamorphosed oceanic crust may be a critical control on megathrust strength and deformation style. However, little is known about the str
The rheology of the metamorphosed oceanic crust may be a critical control on megathrust strength and deformation style. However, little is known about the str
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ee4e0cedac92a4236a39459b8a4ee277
https://pubmed.ncbi.nlm.nih.gov/32518823
https://pubmed.ncbi.nlm.nih.gov/32518823