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- W2738465509 endingPage "106" @default.
- W2738465509 startingPage "87" @default.
- W2738465509 abstract "From the scant Hadean records of the Jack Hills to Cenozoic supervolcanoes, the continental crust provides a synoptic view deep into Earth history. However, the information is fragmented, as large volumes of continental crust have been recycled back into the mantle by a variety of processes. The preserved crustal record is the balance between the volume of crust generated by magmatic processes and the volume destroyed through return to the mantle by tectonic erosion and lower crustal delamination. At present-day, the Earth has reached near-equilibrium between the amount of crust being generated and that being returned to the mantle at subduction zones. However, multiple lines of evidence support secular change in crustal processes through time, including magma compositions, mantle temperatures, and metamorphic gradients. Though a variety of isotopic proxies are used to estimate crustal growth through time, none of those currently utilized are able to quantify the volumes of crust recycled back into the mantle. This implies the estimates of preserved continental crust and growth curves derived therefrom represent only a minimum of total crustal growth. We posit that from the Neoarchean, the probable onset of modern-day style plate tectonics (i.e. steep subduction), there has been no net crustal growth (and perhaps even a net loss) of the continental crust. Deciphering changes from this equilibrium state through geologic time remains a continual pursuit of crustal evolution studies." @default.
- W2738465509 created "2017-07-31" @default.
- W2738465509 creator A5031387958 @default.
- W2738465509 creator A5037339212 @default.
- W2738465509 creator A5060053337 @default.
- W2738465509 date "2017-09-01" @default.
- W2738465509 modified "2023-10-18" @default.
- W2738465509 title "Growth, destruction, and preservation of Earth's continental crust" @default.
- W2738465509 cites W1145830493 @default.
- W2738465509 cites W1482200804 @default.
- W2738465509 cites W1492675645 @default.
- W2738465509 cites W1509769237 @default.
- W2738465509 cites W1520012803 @default.
- W2738465509 cites W1523733318 @default.
- W2738465509 cites W1582566143 @default.
- W2738465509 cites W1676343945 @default.
- W2738465509 cites W1681073458 @default.
- W2738465509 cites W1706860248 @default.
- W2738465509 cites W1777324711 @default.
- W2738465509 cites W178061381 @default.
- W2738465509 cites W1817925888 @default.
- W2738465509 cites W1848614974 @default.
- W2738465509 cites W1855392460 @default.
- W2738465509 cites W1885081053 @default.
- W2738465509 cites W1963870912 @default.
- W2738465509 cites W1965394610 @default.
- W2738465509 cites W1967806476 @default.
- W2738465509 cites W1969845853 @default.
- W2738465509 cites W1971275780 @default.
- W2738465509 cites W1972028040 @default.
- W2738465509 cites W1972081641 @default.
- W2738465509 cites W1972673996 @default.
- W2738465509 cites W1972746128 @default.
- W2738465509 cites W1973876227 @default.
- W2738465509 cites W1974418740 @default.
- W2738465509 cites W1975546571 @default.
- W2738465509 cites W1975676133 @default.
- W2738465509 cites W1975757281 @default.
- W2738465509 cites W1975871169 @default.
- W2738465509 cites W1976449367 @default.
- W2738465509 cites W1978290547 @default.
- W2738465509 cites W1978454692 @default.
- W2738465509 cites W1978464139 @default.
- W2738465509 cites W1980364678 @default.
- W2738465509 cites W1981028951 @default.
- W2738465509 cites W1981072182 @default.
- W2738465509 cites W1981308828 @default.
- W2738465509 cites W1981438127 @default.
- W2738465509 cites W1982925530 @default.
- W2738465509 cites W1983048619 @default.
- W2738465509 cites W1983523676 @default.
- W2738465509 cites W1985583508 @default.
- W2738465509 cites W1986179459 @default.
- W2738465509 cites W1987970271 @default.
- W2738465509 cites W1988484459 @default.
- W2738465509 cites W1988503846 @default.
- W2738465509 cites W1988715580 @default.
- W2738465509 cites W1989445090 @default.
- W2738465509 cites W1989471247 @default.
- W2738465509 cites W1989945922 @default.
- W2738465509 cites W1990480416 @default.
- W2738465509 cites W1990719119 @default.
- W2738465509 cites W1990775613 @default.
- W2738465509 cites W1992565879 @default.
- W2738465509 cites W1993832836 @default.
- W2738465509 cites W1993867360 @default.
- W2738465509 cites W1994010532 @default.
- W2738465509 cites W1994048706 @default.
- W2738465509 cites W1996079372 @default.
- W2738465509 cites W1997233054 @default.
- W2738465509 cites W1998330537 @default.
- W2738465509 cites W1998765219 @default.
- W2738465509 cites W2000320267 @default.
- W2738465509 cites W2004552311 @default.
- W2738465509 cites W2004934899 @default.
- W2738465509 cites W2005571584 @default.
- W2738465509 cites W2005925547 @default.
- W2738465509 cites W2006234070 @default.
- W2738465509 cites W2007139925 @default.
- W2738465509 cites W2008087815 @default.
- W2738465509 cites W2008350311 @default.
- W2738465509 cites W2008787240 @default.
- W2738465509 cites W2009732140 @default.
- W2738465509 cites W2010249788 @default.
- W2738465509 cites W2010259407 @default.
- W2738465509 cites W2010432538 @default.
- W2738465509 cites W2010873910 @default.
- W2738465509 cites W2011161735 @default.
- W2738465509 cites W2011305958 @default.
- W2738465509 cites W2011332054 @default.
- W2738465509 cites W2011549988 @default.
- W2738465509 cites W2011738367 @default.
- W2738465509 cites W2012492236 @default.
- W2738465509 cites W2014359877 @default.
- W2738465509 cites W2014763088 @default.
- W2738465509 cites W2014998287 @default.
- W2738465509 cites W2016855401 @default.
- W2738465509 cites W2017512729 @default.