Matches in SemOpenAlex for { <https://semopenalex.org/work/W4313251965> ?p ?o ?g. }
- W4313251965 abstract "Density instabilities in the lithosphere can founder gravitationally via viscous dripping and decoupling from overlying crust. The lithospheric dripping concept has been invoked across the globe, but the diversity of crustal effects, observable evidence, and tectonic settings involved in dripping remain underexplored. Here, we synthesize numerical and analogue modeling studies and geologic data from the literature, including all proposed lithospheric dripping events to-date. We argue that two distinct styles of dripping can occur depending on crustal strength (relative to that of the mantle lithosphere). Near-surface contraction and subsidence of strong crusts contrasts with near-surface extension and uplift of weak crusts. We discuss these events in terms of tectonic setting, timing, size, and the main types of data associated with each event. We also find that lithospheric dripping is associated with a distinct suite of geological observations including sedimentological, structural, volcanic, and geophysical data, which can be used to distinguish strong crusts from weak crusts. We find 27 events for which lithospheric dripping is a key hypothesis, including 9 with clear evidence for strong-crust dripping and 3 with clear evidence of weak-crust dripping. We review emerging research methods have the potential to detect the signals of dripping in the geologic and geophysical record, and we suggest additional techniques in light of our strong-crust versus weak-crust framework. The diverse tectonic settings and inferred consequences of these lithospheric drips, if confirmed, would demand a shift in our understanding of continental geology to emphasize the role of vertical removal of continental lithosphere." @default.
- W4313251965 created "2023-01-06" @default.
- W4313251965 creator A5079003322 @default.
- W4313251965 creator A5091198232 @default.
- W4313251965 date "2023-02-01" @default.
- W4313251965 modified "2023-09-27" @default.
- W4313251965 title "Diverse Styles of Lithospheric Dripping: Synthesizing Gravitational Instability Models, Continental Tectonics, and Geologic Observations" @default.
- W4313251965 cites W1525355917 @default.
- W4313251965 cites W1543257786 @default.
- W4313251965 cites W1545002229 @default.
- W4313251965 cites W1570665500 @default.
- W4313251965 cites W1641796164 @default.
- W4313251965 cites W1650192457 @default.
- W4313251965 cites W1664416090 @default.
- W4313251965 cites W1685029859 @default.
- W4313251965 cites W1829440104 @default.
- W4313251965 cites W1836012059 @default.
- W4313251965 cites W1842190251 @default.
- W4313251965 cites W1876965659 @default.
- W4313251965 cites W1937741642 @default.
- W4313251965 cites W1951893631 @default.
- W4313251965 cites W1963507821 @default.
- W4313251965 cites W1963541902 @default.
- W4313251965 cites W1964286915 @default.
- W4313251965 cites W1964625886 @default.
- W4313251965 cites W1966167298 @default.
- W4313251965 cites W1966540505 @default.
- W4313251965 cites W1967337985 @default.
- W4313251965 cites W1968024446 @default.
- W4313251965 cites W1968409103 @default.
- W4313251965 cites W1969469243 @default.
- W4313251965 cites W1970035256 @default.
- W4313251965 cites W1970046233 @default.
- W4313251965 cites W1971173267 @default.
- W4313251965 cites W1971927938 @default.
- W4313251965 cites W1974882281 @default.
- W4313251965 cites W1976894814 @default.
- W4313251965 cites W1977163158 @default.
- W4313251965 cites W1978087001 @default.
- W4313251965 cites W1983529616 @default.
- W4313251965 cites W1983660516 @default.
- W4313251965 cites W1985176040 @default.
- W4313251965 cites W1986699878 @default.
- W4313251965 cites W1987262941 @default.
- W4313251965 cites W1988841624 @default.
- W4313251965 cites W1989445090 @default.
- W4313251965 cites W1990496883 @default.
- W4313251965 cites W1992299314 @default.
- W4313251965 cites W1994048706 @default.
- W4313251965 cites W1995024114 @default.
- W4313251965 cites W1995115331 @default.
- W4313251965 cites W1997255700 @default.
- W4313251965 cites W1997706103 @default.
- W4313251965 cites W1999125016 @default.
- W4313251965 cites W2003243667 @default.
- W4313251965 cites W2005746725 @default.
- W4313251965 cites W2007472247 @default.
- W4313251965 cites W2008412316 @default.
- W4313251965 cites W2008787240 @default.
- W4313251965 cites W2009279133 @default.
- W4313251965 cites W2014969794 @default.
- W4313251965 cites W2016613347 @default.
- W4313251965 cites W2017865819 @default.
- W4313251965 cites W2024998721 @default.
- W4313251965 cites W2025179369 @default.
- W4313251965 cites W2028100646 @default.
- W4313251965 cites W2029536264 @default.
- W4313251965 cites W2030688224 @default.
- W4313251965 cites W2033947516 @default.
- W4313251965 cites W2033955470 @default.
- W4313251965 cites W2035774436 @default.
- W4313251965 cites W2035867684 @default.
- W4313251965 cites W2037812149 @default.
- W4313251965 cites W2038999786 @default.
- W4313251965 cites W2039016697 @default.
- W4313251965 cites W2039910985 @default.
- W4313251965 cites W2041331473 @default.
- W4313251965 cites W2042286328 @default.
- W4313251965 cites W2042654809 @default.
- W4313251965 cites W2043464556 @default.
- W4313251965 cites W2043695697 @default.
- W4313251965 cites W2045066141 @default.
- W4313251965 cites W2045479126 @default.
- W4313251965 cites W2045775785 @default.
- W4313251965 cites W2047093010 @default.
- W4313251965 cites W2047634839 @default.
- W4313251965 cites W2048286776 @default.
- W4313251965 cites W2048564681 @default.
- W4313251965 cites W2049451277 @default.
- W4313251965 cites W2049575148 @default.
- W4313251965 cites W2051007960 @default.
- W4313251965 cites W2051303926 @default.
- W4313251965 cites W2052907420 @default.
- W4313251965 cites W2053090923 @default.
- W4313251965 cites W2053211094 @default.
- W4313251965 cites W2053463528 @default.
- W4313251965 cites W2055173044 @default.
- W4313251965 cites W2055412715 @default.
- W4313251965 cites W2057408414 @default.
- W4313251965 cites W2057810794 @default.