FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W809600265> ?p ?o ?g. }

• W809600265 endingPage "133" @default.
• W809600265 startingPage "119" @default.
• W809600265 abstract "The presence of hot, weak crust is a central component of recent hypotheses that seek to explain the evolution of continent-continent collisions, and in particular may play an important role in accommodating the >3000 km of convergence within the Himalaya–Tibetan collision over the last ∼55 Myr. Models that implicate flow of semi-viscous midcrustal rocks south toward the front of the Himalayan orogen, ‘channel flow’, are able to account for many geologic observations in the Himalaya, while alternative models of collision, particularly ‘thrust-wedge taper’, demonstrate that much of the observed geology could have formed in the absence of a low-viscosity mid-crustal layer. Several recent studies, synthesized here, have prompted a shift from initial assumptions that channel flow and thrust-wedge taper processes are by definition mutually exclusive. These new studies reveal the presence of several tectonometamorphic discontinuities in the midcrust that appear to reflect a continuum of deformation in which both channel- and wedge-type processes operate in spatially and temporally distinct domains within the orogen, and further, that the system may migrate back and forth between these types of behavior. This continuum of deformation styles within the collisional system is of crucial importance for explaining the evolution of the Himalayan orogen and, hence, for understanding the evolution of Earth's many continent-continent collision zones." @default.
• W809600265 created "2016-06-24" @default.
• W809600265 creator A5009741234 @default.
• W809600265 creator A5024788787 @default.
• W809600265 creator A5042808288 @default.
• W809600265 date "2015-09-01" @default.
• W809600265 modified "2023-10-05" @default.
• W809600265 title "How does the mid-crust accommodate deformation in large, hot collisional orogens? A review of recent research in the Himalayan orogen" @default.
• W809600265 cites W1491482336 @default.
• W809600265 cites W1494846356 @default.
• W809600265 cites W1524459215 @default.
• W809600265 cites W1528695685 @default.
• W809600265 cites W1538686567 @default.
• W809600265 cites W1583058920 @default.
• W809600265 cites W1596863264 @default.
• W809600265 cites W1658256170 @default.
• W809600265 cites W1665972339 @default.
• W809600265 cites W1816648696 @default.
• W809600265 cites W1861675434 @default.
• W809600265 cites W1870803485 @default.
• W809600265 cites W1931141686 @default.
• W809600265 cites W1939462715 @default.
• W809600265 cites W1941090763 @default.
• W809600265 cites W1964129853 @default.
• W809600265 cites W1965732067 @default.
• W809600265 cites W1968718157 @default.
• W809600265 cites W1968923199 @default.
• W809600265 cites W1969231900 @default.
• W809600265 cites W1971707699 @default.
• W809600265 cites W1971728771 @default.
• W809600265 cites W1971953156 @default.
• W809600265 cites W1976307868 @default.
• W809600265 cites W1976339167 @default.
• W809600265 cites W1976467450 @default.
• W809600265 cites W1977382752 @default.
• W809600265 cites W1980434258 @default.
• W809600265 cites W1981421896 @default.
• W809600265 cites W1982985939 @default.
• W809600265 cites W1984200080 @default.
• W809600265 cites W1984360620 @default.
• W809600265 cites W1984724289 @default.
• W809600265 cites W1987562178 @default.
• W809600265 cites W1989601679 @default.
• W809600265 cites W1989832452 @default.
• W809600265 cites W1989908130 @default.
• W809600265 cites W1992096405 @default.
• W809600265 cites W1993827822 @default.
• W809600265 cites W1996081112 @default.
• W809600265 cites W1997744066 @default.
• W809600265 cites W1998030192 @default.
• W809600265 cites W2002088894 @default.
• W809600265 cites W2003419666 @default.
• W809600265 cites W2004480847 @default.
• W809600265 cites W2006280751 @default.
• W809600265 cites W2008413745 @default.
• W809600265 cites W2009145927 @default.
• W809600265 cites W2009196217 @default.
• W809600265 cites W2009383297 @default.
• W809600265 cites W2015912791 @default.
• W809600265 cites W2015923510 @default.
• W809600265 cites W2018576204 @default.
• W809600265 cites W2018637715 @default.
• W809600265 cites W2018693288 @default.
• W809600265 cites W2019382148 @default.
• W809600265 cites W2019946678 @default.
• W809600265 cites W2020159892 @default.
• W809600265 cites W2021856487 @default.
• W809600265 cites W2024256007 @default.
• W809600265 cites W2024860961 @default.
• W809600265 cites W2024969161 @default.
• W809600265 cites W2027243914 @default.
• W809600265 cites W2027508217 @default.
• W809600265 cites W2027692487 @default.
• W809600265 cites W2029429267 @default.
• W809600265 cites W2030197879 @default.
• W809600265 cites W2030347033 @default.
• W809600265 cites W2030721727 @default.
• W809600265 cites W2031857048 @default.
• W809600265 cites W2033136921 @default.
• W809600265 cites W2034091664 @default.
• W809600265 cites W2036255205 @default.
• W809600265 cites W2046223350 @default.
• W809600265 cites W2046809141 @default.
• W809600265 cites W2050487135 @default.
• W809600265 cites W2052998128 @default.
• W809600265 cites W2054314513 @default.
• W809600265 cites W2054541681 @default.
• W809600265 cites W2055356153 @default.
• W809600265 cites W2056277042 @default.
• W809600265 cites W2057095026 @default.
• W809600265 cites W2057405293 @default.
• W809600265 cites W2059912112 @default.
• W809600265 cites W2061313115 @default.
• W809600265 cites W2061693276 @default.
• W809600265 cites W2062706977 @default.
• W809600265 cites W2067336156 @default.
• W809600265 cites W2070699711 @default.
• W809600265 cites W2071737204 @default.

• next