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Geology of the Henty Fault Wedge, Western Tasmania
1993The Henty Fault Wedge is a misfit slice of Cambrian lithologies which have been fault emplaced into the middle to late Cambrian Mt Read Volcanics. The Henty Fault Wedge has an exposed area of 30km\\(^2\\) and is located midway between Queenstown and Rosebery in western Tasmania (Fig 1).
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The Geology of a Portion of the Redlands Quadrangle, California : a Study in Faulting
1931The San Andreas Rift after passing through the Cajon Pass in Southern California proceeds approximately S 60° E along the base of the San Bernardino Mountains which rise to the north. About eight miles east of the city of Redlands, Mill Creek issues from the San Bernardino Mountains south-west on to the alluvium covered flood plain. Four miles to the
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Frictional-viscous flow, seismicity and the geology of weak faults: a review and future directions
Geological Society, London, Special Publications, 2008Abstract Previously hypothesized fault weakening mechanisms include faults lined by low-friction clay gouges, elevated pore pressures within fault cores and/or the operation of dynamic weakening during seismic slip. Geological studies to support dynamic weakening are still in their infancy and there is little geological evidence for the ...
Imber, Jonathan +4 more
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Relations Among Fault Behavior, Subsurface Geology, and Three-Dimensional Velocity Models
Science, 1991The development of three-dimensional P-wave velocity models for the regions surrounding five large earthquakes in California has lead to the recognition of relations among fault behavior and the material properties of the rocks that contact the fault at seismogenic depths; regions of high moment release appear to correlate with high seismic velocities ...
A J, Michael, D, Eberhart-Phillips
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The Alpine Fault, New Zealand: Surface geology and field relationships
2007The Alpine Fault forms part of the on-land Pacific-Australian plate boundary. Generally the fault has a simple straight trace, striking ca. 055° and dipping moderately eastwards, but in central areas it is serially partitioned. Late Quaternary strike-slip rates are 23-25 mm/yr, but dip-slip rates range from ca.
Richard J. Norris, Alan F. Cooper
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Geology of the almus fault zone (AFZ) (Almus-Tokat)
2020ALMÜS FAY KUŞA?I' NIN JELOJÎSÎ (ALMUS - TOKAT) Bozkurt, Erdin Mühendislik Fakültesi Jeloji Mühendisliği Bölümü, Y. Lisans Tezi Tez Yöneticisi: Prof. Dr. Ali Kocyigit 118 Sayfa, Şubat 1990 ÖZET Çalışma alanı Almus ile Tokat arasında yer alır. inceleme alanında yüzeyleyen kaya stratigrafi birimleri temel ve örtü kayaları olmak üzere iki ana gruba ...
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The Geology of the Arakapas Fault Belt Area Troodas Massif, Cyprus
1975A wide variety of geological evidence supports the contention that the Troodos massif, Cyprus is a fragment of Mesozoic sea-floor created at a constructive plate margin. Here the geology of an east-west striking fault zone in the southern part of the massif, the Arakapas Fault Belt (APB), is investigated and evidence is presented which supports its ...
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STRUKTUR GEOLOGI - WRENCH FAULTS , DAN MINERALISASI
2020Ramaniya Ramadhani, Stevanus Nalendra
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A Note on the Geology and Fault Systems of Krishnagiri Area
Journal Geological Society of India, 1971V. M. Moralev +2 more
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