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Lower crustal delamination and evolution of continental crust

Shan, Gao and Ducea, Mihai N. and Zhenmin, Jin and Saleeby, Jason (1998) Lower crustal delamination and evolution of continental crust. Geological Journal of China Universities, 4 (3). pp. 241-249. ISSN 1006-7493.

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It has been suggested that during collision events leading to crustal thickening and formation of eclogite, or through underplating and fractionation of basaltic magma at the base of the crust, the mafic/ultramafic root of the continental crust will become denser than the underlying upper mantle. This density instability will lead to delamination that occurs during continental collision and drives lower crust recycling into the mantle. Lower crustal delamination has been proposed to explain the dilemma that the primary mantle additions into the crust are principally basaltic, whereas the present-day continental crust has an intermediate bulk composition. Eu, Sr and transition metals (Cr, Ni, Co, V, Sc and Ti) are enriched in mafic granulites and eclogites. As a result, delamination of lower crust will reduce abundances of these elements as well as Eu/Eu* and ratios of Sr and transition metals to Nd in the continental crust. Correspondingly, SiO_2 increases. Therefore, Eu, Sr and transition metals can be used together to test the consistency of a geochemical model of lower crustal delamination. The seismic consequence of delamination will be evident in lower seismic velocities due to the loss of high-velocity mafic root, while geologically, delamination is expected to produce crustal exhumation followed by extension and formation of basins and leads to a lack of substantial mountain roots. Our estimates of the total crust composition in central East China show a more evolved character compared to models of Rudnick and Fountain (1995) and Taylor and McLennan (1985, 1995) and are characterized by a prominent negative Eu anomaly (Eu/Eu* = 0.80), higher SiO_2 (61.8%), and lower Sr/Nd (~10) as well as lower Sr/Nd, Cr/Nd, Ni/Nd, Co/Nd, V/Nd and Ti/Nd ratios. This, together with slower crustal velocities and remarkably thin crustal thicknesses (34km) for the paleozoic-Mesozoic Qinling-Dabie orogenic belt, leads to the suggestion that lower crustal delamination played an important role in modification of the East China crust. Mass balance modeling further suggests that eclogite from the Dabie-Sulu ultrahigh pressure metamorphic belt is the most likely candidate as the delaminated material, and that a cumulative 37~82km thick eclogitic lower crust is required to have been delaminated in order to explain the relative Eu, Sr and transition metal deficits in the crust of central East China. Delamination of eclogites can also explain the significantly higher than eclogite Poisson's ratio in the present Dabie lower crust and upper mantle and lack of eclogite in Cenozoic xenolith populations of the lower crust and upper mantle in East China. As an analogue, xenolith and geophysical evidences from the Sierra Nevada batholith indicate existence of a ~70km mafic-ultramafic eclogite facies root in Mid-Miocene, which complements the ~30km granitic intrusion as cumulates/residues. Delamination of the thick eclogitic root has also been proposed to explain the very thin crust of 30~40km currently in the southern Sierra Nevada, which is mainly granitic, as indicated by Vp=6.0~6.3km s^(-1), and is underlain by a peridotitic upper mantle, as revealed by younger Late Miocene xenoliths. Therefore, delamination of eclogite is a common and important process for evolution of continental crust and crust-mantle interaction.

Item Type:Article
Ducea, Mihai N.0000-0002-5322-0782
Additional Information:© 1998 China Academic Journals.
Subject Keywords:delamination, lower crust, crust-mantle interaction, Qinling-Dabie orogenic belt, Sierra Nevada batholith
Issue or Number:3
Record Number:CaltechAUTHORS:20140822-072911268
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Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:48788
Deposited By: Tony Diaz
Deposited On:22 Aug 2014 15:32
Last Modified:09 Mar 2020 13:18

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