Matches in SemOpenAlex for { <https://semopenalex.org/work/W2033178207> ?p ?o ?g. }
- W2033178207 endingPage "20" @default.
- W2033178207 startingPage "11" @default.
- W2033178207 abstract "Fault generated melt, pseudotachylyte, is an established indicator of palaeoseismic faulting. The existing consensus that frictionally induced melting occurs within the classic seismogenic zone contrast the contention over how pseudotachylyte forms within the ductile regime. Central to this issue is whether all pseudotachylyte originates as pressure-dependent frictional melt along slip surfaces, or if pressure-independent processes have roles in its formation. Propagation of high-velocity slip into deeper crustal levels provides a satisfactory explanation for pseudotachylyte at depth, but does not of itself rationalize earthquake nucleation outside the classic seismogenic zone. Pseudotachylyte from the Minas Fault Zone, Nova Scotia, Canada is used to demonstrate the formation and preservation of fault-related melt under lower crustal conditions. Microstructures retain evidence of intense dislocation glide with minimal climb, and ductile disaggregation of the host; the latter are consistent with intracrystalline deformation in the Peierls stress-controlled glide regime. It remains unclear whether the crystal plasticity serves only as a precursory stage to rupture and high-velocity slip or is itself responsible for both instability and the thermal transient. There are similarities between accelerating plastic slip leading to rupture and aseismic creep bursts (tremor) that emphasize the mechanistic complexity of deep faulting, and the need to extend consideration beyond that of a simple brittle-ductile response. The occurrence of tremor bursts fall within the depth range of “paradoxical” pseudotachylyte and provides a circumstantial link between active tectonics and the geologic record that merits examination." @default.
- W2033178207 created "2016-06-24" @default.
- W2033178207 creator A5055530012 @default.
- W2033178207 date "2012-05-01" @default.
- W2033178207 modified "2023-10-11" @default.
- W2033178207 title "Paradoxical pseudotachylyte – Fault melt outside the seismogenic zone" @default.
- W2033178207 cites W1965321620 @default.
- W2033178207 cites W1969020175 @default.
- W2033178207 cites W1972346514 @default.
- W2033178207 cites W1972382121 @default.
- W2033178207 cites W1975088312 @default.
- W2033178207 cites W1976229064 @default.
- W2033178207 cites W1977156689 @default.
- W2033178207 cites W1980824982 @default.
- W2033178207 cites W1980953962 @default.
- W2033178207 cites W1981728806 @default.
- W2033178207 cites W1982217242 @default.
- W2033178207 cites W1984964257 @default.
- W2033178207 cites W1985119459 @default.
- W2033178207 cites W1987858217 @default.
- W2033178207 cites W1989246055 @default.
- W2033178207 cites W1991764107 @default.
- W2033178207 cites W1992503071 @default.
- W2033178207 cites W1994430007 @default.
- W2033178207 cites W1994635685 @default.
- W2033178207 cites W1996123535 @default.
- W2033178207 cites W1997698132 @default.
- W2033178207 cites W1998445318 @default.
- W2033178207 cites W2002543944 @default.
- W2033178207 cites W2004040934 @default.
- W2033178207 cites W2005568531 @default.
- W2033178207 cites W2010446848 @default.
- W2033178207 cites W2010773113 @default.
- W2033178207 cites W2011939763 @default.
- W2033178207 cites W2012292189 @default.
- W2033178207 cites W2016834726 @default.
- W2033178207 cites W2016966890 @default.
- W2033178207 cites W2017274089 @default.
- W2033178207 cites W2018282504 @default.
- W2033178207 cites W2018624703 @default.
- W2033178207 cites W2025968992 @default.
- W2033178207 cites W2027147653 @default.
- W2033178207 cites W2029168449 @default.
- W2033178207 cites W2036453731 @default.
- W2033178207 cites W2042767874 @default.
- W2033178207 cites W2045984175 @default.
- W2033178207 cites W2046754399 @default.
- W2033178207 cites W2048167361 @default.
- W2033178207 cites W2049187645 @default.
- W2033178207 cites W2049578514 @default.
- W2033178207 cites W2051100781 @default.
- W2033178207 cites W2052134023 @default.
- W2033178207 cites W2053813145 @default.
- W2033178207 cites W2057785739 @default.
- W2033178207 cites W2058229804 @default.
- W2033178207 cites W2060274387 @default.
- W2033178207 cites W2061928350 @default.
- W2033178207 cites W2061976920 @default.
- W2033178207 cites W2068462039 @default.
- W2033178207 cites W2068493511 @default.
- W2033178207 cites W2069168481 @default.
- W2033178207 cites W2071944322 @default.
- W2033178207 cites W2074311691 @default.
- W2033178207 cites W2077067150 @default.
- W2033178207 cites W2081843634 @default.
- W2033178207 cites W2083339205 @default.
- W2033178207 cites W2083901848 @default.
- W2033178207 cites W2090412346 @default.
- W2033178207 cites W2092227172 @default.
- W2033178207 cites W2092464363 @default.
- W2033178207 cites W2092630124 @default.
- W2033178207 cites W2093569101 @default.
- W2033178207 cites W2107419027 @default.
- W2033178207 cites W2111091385 @default.
- W2033178207 cites W2112214252 @default.
- W2033178207 cites W2113585222 @default.
- W2033178207 cites W2117221055 @default.
- W2033178207 cites W2119194686 @default.
- W2033178207 cites W2123302430 @default.
- W2033178207 cites W2126862123 @default.
- W2033178207 cites W2126979131 @default.
- W2033178207 cites W2144940781 @default.
- W2033178207 cites W2145984304 @default.
- W2033178207 cites W2147474159 @default.
- W2033178207 cites W2147984970 @default.
- W2033178207 cites W2148872613 @default.
- W2033178207 cites W2150630554 @default.
- W2033178207 cites W2151492534 @default.
- W2033178207 cites W2155128667 @default.
- W2033178207 cites W2161527086 @default.
- W2033178207 cites W2164683099 @default.
- W2033178207 cites W2165149348 @default.
- W2033178207 cites W2169827520 @default.
- W2033178207 cites W2170219059 @default.
- W2033178207 cites W3043123853 @default.
- W2033178207 cites W4237807282 @default.
- W2033178207 doi "https://doi.org/10.1016/j.jsg.2011.11.016" @default.
- W2033178207 hasPublicationYear "2012" @default.