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Tectonophysics, ISSN 0040-1951, 10/2012, Volume 574-575, pp. 1 - 71
Journal Article
Geophysical Research Letters, ISSN 0094-8276, 11/2015, Volume 42, Issue 22, pp. 9772 - 9780
The Dead Sea is a prime location to study the structure and development of pull‐apart basins. We analyzed tomographic models of Vp, Vs, and Vp/Vs using... 
Vp, Vp/Vs tomography | Dead Sea basin | self‐organizing maps | pull‐apart basin | joint interpretation | self-organizing maps | pull-apart basin | V | tomography | GEOSCIENCES, MULTIDISCIPLINARY | RIFT | AREA | MODELS | CRUSTAL STRUCTURE | COAST RANGES | CLASSIFICATION | DEFORMATION | PULL-APART | LITHOLOGY | Tomography | Sediments | Neural networks | Basins | Basements | Signatures | Clustering | Seismicity | Crystal structure
Journal Article
Journal of Geophysical Research: Solid Earth, ISSN 2169-9313, 03/2017, Volume 122, Issue 3, pp. 2193 - 2218
Paleoseismic data on the timing of ground‐rupturing earthquakes constrain the recurrence behavior of active faults and can provide insight on the rupture... 
Frazier Mountain | paleoseismology | rupture history | pull‐apart basin | pull-apart basin
Journal Article
Tectonics, ISSN 0278-7407, 01/2018, Volume 37, Issue 1, pp. 343 - 358
Journal Article
Geological Journal, ISSN 0072-1050, 03/2015, Volume 50, Issue 2, pp. 139 - 156
Journal Article
Journal of Geophysical Research: Solid Earth, ISSN 0148-0227, 01/2012, Volume 117, Issue B1, p. n/a
Pull‐apart basins are narrow zones of crustal extension bounded by strike‐slip faults that can serve as analogs to the early stages of crustal rifting. We use... 
North Sea | retrorgrade metamorphism | basin subsidence | pull‐apart basin | muscovite | transform fault | GEOCHEMISTRY & GEOPHYSICS | CONTINENTAL-MARGIN | EVOLUTION | NORTH | SEISMIC-REFRACTION | AQUEOUS FLUIDS | STRAIN LOCALIZATION | MANTLE FLUIDS | TRANSFORM | FAULT | PULL-APART BASINS | Petrology | Rheology | Mineralogy | Geodetics | Plate tectonics | Sedimentary geology | Gravity
Journal Article
Journal of Asian Earth Sciences, ISSN 1367-9120, 2007, Volume 29, Issue 2, pp. 253 - 265
Journal Article
Geochemistry, Geophysics, Geosystems, ISSN 1525-2027, 12/2011, Volume 12, Issue 12, pp. 1 - n/a
The Owen Fracture Zone is a 800 km‐long fault system that accommodates the dextral strike‐slip motion between India and Arabia plates. Because of slow pelagic... 
Indian Ocean | Owen Fracture Zone | pull‐apart | transform fault | pull-apart | INDUS FAN | EXTENSION | NORTHERN ARABIAN SEA | MOTIONS | DEAD-SEA BASIN | GEOCHEMISTRY & GEOPHYSICS | ANATOLIAN FAULT | TRANSFORM | PULL-APART BASINS | DALRYMPLE TROUGH | TECTONIC EVOLUTION | Plate tectonics | Marine geology | Geophysics | Earth Sciences | Sciences of the Universe | Tectonics | Environmental Sciences | Global Changes
Journal Article
Geochemistry Geophysics Geosystems, ISSN 1525-2027, 07/2008, Volume 9, Issue 7, pp. Q07009 - n/a
The Dead Sea fault (DSF) plate boundary has accommodated relative sinistral motion between the Sinai and Arabian plates since the Neogene. Geologically based... 
Continental tectonics |