Results 61 to 70 of about 576,763 (311)
The role of coseismic Coulomb stress changes in shaping the hard-link between normal fault segments [PDF]
, 2017 The mechanism and evolution of fault linkage is important in the growth and development of large faults. Here we investigate the role of coseismic stress changes in shaping the hard-links between parallel normal fault segments (or faults), by comparing ...
Biggs, J., Fagereng, Ake, Hodge, Michael
core +4 more sources
Half graben versus large‐offset low‐angle normal fault: Importance of keeping cool during normal faulting [PDF]
Journal of Geophysical Research: Solid Earth, 2002 We study the effect of temperature in the crust on the style of faulting during the extension of a model lithosphere. Two distinct fault patterns are seen depending on whether the brittle layer thickness HL is greater or less than a critical value HC.
Lavier, L., Buck, W.
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FEBS Letters, EarlyView.We reconstituted Synechocystis glycogen synthesis in vitro from purified enzymes and showed that two GlgA isoenzymes produce glycogen with different architectures: GlgA1 yields denser, highly branched glycogen, whereas GlgA2 synthesizes longer, less‐branched chains.
Kenric Lee +3 more
wiley +1 more source
Sliding modes of fault activation under constant normal stiffness conditions
Journal of Rock Mechanics and Geotechnical Engineering, 2023 Fault activation has been the focus of research community for years. However, the studies of fault activation remain immature, such as the fault activation mode and its major factors under constant normal stiffness (CNS) conditions associated with large ...
Chuanqing Zhang +5 more
doaj +1 more source
Simulation of rock salt dissolution and its impact on land subsidence [PDF]
, 2013 Extensive land subsidence can occur due to subsurface dissolution of evaporites such as halite and gypsum. This paper explores techniques to simulate the salt dissolution forming an intrastratal karst, which is embedded in a sequence of carbonates, marls,
Huggenberger, P. +3 more
core +2 more sources
FEBS Letters, EarlyView.We identified a systemic, progressive loss of protein S‐glutathionylation—detected by nonreducing western blotting—alongside dysregulation of glutathione‐cycle enzymes in both neuronal and peripheral tissues of Taiwanese SMA mice. These alterations were partially rescued by SMN antisense oligonucleotide therapy, revealing persistent redox imbalance as ...
Sofia Vrettou, Brunhilde Wirth
wiley +1 more source
Fault slip-rate variations during crustal-scale strain localisation, central Italy [PDF]
, 2002 Rates of plate motion are generally uniform over 10–102 Myrs timescales. Faults between tectonic plates might, therefore, be expected to show temporally-uniform slip-rates if the same number of faults remain active. For an extending region of the Eurasia-
Cowie, P +4 more
core
Strain compatibility and fault linkage in relay zones on normal faults [PDF]
Journal of Structural Geology, 2012 Relay zones on normal faults are unlikely to have tabular geometries as depicted in idealised models. Rotation of a relay ramp between non-parallel and non-planar relay-bounding faults will inevitably lead to strain compatibility problems causing open gaps or overlaps within the relay zone. Linkage of relay-bounding faults does not evolve from a single
Long, J.J., Imber, J.
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β‐TrCP overexpression enhances cisplatin sensitivity by depleting BRCA1
Molecular Oncology, EarlyView.Low levels of β‐TrCP (Panel A) allow the accumulation of BRCA1 and CtIP, which facilitate the repair of cisplatin‐induced DNA damage via homologous recombination (HR) and promote tumor cell survival. In contrast, high β‐TrCP expression (Panel B) leads to BRCA1 and CtIP degradation, impairing HR repair, resulting in persistent DNA damage and apoptosis ...
Rocío Jiménez‐Guerrero +8 more
wiley +1 more source
, 1981 The importance of listric normal faults in the formation of sedimentary basins is becoming increasingly more obvious. Based on reflection seismic sections and surface observations, the following genetic types may be differentiated: - listric normal faults involving the basement that are associated with some crustal attenuation. Such faults occur during
Bally, A W +3 more
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