Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Darrell W. Sims"'
Autor:
Robert T. Pappalardo, S. L. Colton, Geoffrey C. Collins, Danielle Y. Wyrick, Darrell W. Sims, David A. Ferrill, Alan P. Morris
Publikováno v:
Geophysical Research Letters. 41:3774-3778
Grooved terrain on Ganymede consists of distinct areas of parallel to subparallel ridges and troughs at a variety of spatial scales. Grooved terrain has been interpreted as the product of tectonism in the form of fault-accommodated distributed lithos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::326c98cff33865c0be73d8f2b7921b8a
https://doi.org/10.1002/2014gl060359
https://doi.org/10.1002/2014gl060359
Autor:
Nathan M. Franklin, Darrell W. Sims, Alan P. Morris, Emily J. Beverly, Yoshihiko Tamura Umezawa, S. L. Colton, Danielle Y. Wyrick, David A. Ferrill, Deborah J. Waiting, Mamoru Takanashi
Publikováno v:
AAPG Bulletin. 97:877-898
We study the effects of planform dome shape on fault patterns developing with and without concurrent regional extension oriented oblique to the long axis of the dome. The motivation was the need to understand fault and fracture patterns in two adjace
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9499c3480ffdf03e7a2487a1970c7114
https://doi.org/10.1306/02101209136
https://doi.org/10.1306/02101209136
Autor:
Gloria Eisenstadt, Darrell W. Sims
Publikováno v:
Journal of Structural Geology. 27:1399-1412
Dry sand and wet clay are the most frequently used materials for physical modeling of brittle deformation. We present a series of experiments that shows when the two materials can be used interchangeably, document the differences in deformation patte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6cc64a2d3a0f1b35d6a2afc987b13e95
https://doi.org/10.1016/j.jsg.2005.04.010
https://doi.org/10.1016/j.jsg.2005.04.010
Publikováno v:
Journal of Structural Geology. 21:1027-1038
Large normal faults are corrugated. Corrugations appear to form from overlapping or en echelon fault arrays by two breakthrough mechanisms: lateral propagation of curved fault-tips and linkage by connecting faults. Both mechanisms include localized f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b0bd637ac86cf549cbc3b10132fdab4e
https://doi.org/10.1016/s0191-8141(99)00017-6
https://doi.org/10.1016/s0191-8141(99)00017-6
Publikováno v:
Journal of Structural Geology. 21:533-554
Traditional models describe pull-apart basins as graben or half-graben basins with normal or normal-oblique slip master faults, analogous to Death Valley, California. Yet many pull-aparts are characterized by asymmetric basins with strike-slip master
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe49343e7900e7e8c616f46bf74b1e6f
https://doi.org/10.1016/s0191-8141(99)00010-3
https://doi.org/10.1016/s0191-8141(99)00010-3
Publikováno v:
Water Resources Research. 44
[1] Field investigations of stratified alluvial deposits suggest that they can give rise to a hierarchy of permeability modes across scales, corresponding to a hierarchy of sedimentary unit types and thus may lead to enhanced plume spread in such med
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::384b2288f808ec1bf5e66deb8e4e2618
https://doi.org/10.1029/2007wr006119
https://doi.org/10.1029/2007wr006119
Publikováno v:
Journal of Geophysical Research. 109
[1] Pit craters are circular to elliptical depressions found in alignments (chains), which in many cases coalesce into linear troughs. They are common on the surface of Mars and similar to features observed on Earth and other terrestrial bodies. Pit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::109317179281a19300187b215d61cfaa
https://doi.org/10.1029/2004je002240
https://doi.org/10.1029/2004je002240
Publikováno v:
AAPG Bulletin. 84
Normal faults commonly develop in two oppositely dipping sets having dihedral angles of around 60o, collectively referred to as conjugate normal faults. Conjugate normal faults form at a range of scales from cm to km. Where conjugate normal faults cr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2485014071683149eb915c7089c468b9
https://doi.org/10.1306/8626bef7-173b-11d7-8645000102c1865d
https://doi.org/10.1306/8626bef7-173b-11d7-8645000102c1865d
Publikováno v:
GSA Today. 15:11
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::216bc5b3bed2213543e954d219c1d86c
https://doi.org/10.1130/1052-5173(2005)15<11b:dfsapc>2.0.co
https://doi.org/10.1130/1052-5173(2005)15<11b:dfsapc>2.0.co
Publikováno v:
GSA Today. 14:4
Pit crater chains that are parallel or collinear with normal faults are common on Mars, but only rarely observed on Earth. We explore the origin of pit crater chains using recent high-resolution imagery from Mars, laboratory simulation of pit chains,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::06637aa74337dbbfcac92aae701dec94
https://doi.org/10.1130/1052-5173(2004)014<4:dfsapc>2.0.co
https://doi.org/10.1130/1052-5173(2004)014<4:dfsapc>2.0.co