Generation of continental adakitic rocks: crystallization modeling with variable bulk partition coefficients

Research output: Contribution to journalArticleResearchpeer-review

Abstract

The geochemical signatures (i.e., high Sr/Y and La/Yb ratios) of adakitic rocks in continental settings, which are derived from the continental lower crust rather than from subducted slabs, may reflect high-pressure melting in the lower crust or may be inherited from their sources. The North China Craton (NCC) is an ideal place for investigation of this type of adakites due to its ubiquitous distribution. As an example, we explore the petrogenesis of the Jurassic (~ 163 Ma) adakitic rocks in western Liaoning, in the NE part of the NCC, using elemental and Sr–Nd isotopic analysis and crystallization modeling based on Rhyolite-MELTS. The modeling demonstrates that adakitic signatures can be generated by fractional crystallization of magmas within crust of normal thickness (i.e., 33 km). Partial-melting modeling based on the composition of the lower continental crust shows that only the adakitic rocks from orogenic belts require a thickened crust (i.e., 45 km). We suggest that continental adakitic rocks are not necessarily linked to high-pressure processes and their use as an indicator of thickened/delaminated continental crust should be regarded with caution.

LanguageEnglish
Pages222-231
Number of pages10
JournalLithos
Volume272-273
DOIs
Publication statusPublished - Feb 2017

Fingerprint

Crystallization
partition coefficient
crystallization
Rocks
lower crust
continental crust
rock
modeling
craton
Melting
crust
isotopic analysis
petrogenesis
rhyolite
orogenic belt
fractional crystallization
partial melting
slab
melting
Jurassic

Keywords

  • Continental adakitic rocks
  • Variable bulk partition coefficients
  • Continental crustal thickness
  • North China Craton

Cite this

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title = "Generation of continental adakitic rocks: crystallization modeling with variable bulk partition coefficients",
abstract = "The geochemical signatures (i.e., high Sr/Y and La/Yb ratios) of adakitic rocks in continental settings, which are derived from the continental lower crust rather than from subducted slabs, may reflect high-pressure melting in the lower crust or may be inherited from their sources. The North China Craton (NCC) is an ideal place for investigation of this type of adakites due to its ubiquitous distribution. As an example, we explore the petrogenesis of the Jurassic (~ 163 Ma) adakitic rocks in western Liaoning, in the NE part of the NCC, using elemental and Sr–Nd isotopic analysis and crystallization modeling based on Rhyolite-MELTS. The modeling demonstrates that adakitic signatures can be generated by fractional crystallization of magmas within crust of normal thickness (i.e., 33 km). Partial-melting modeling based on the composition of the lower continental crust shows that only the adakitic rocks from orogenic belts require a thickened crust (i.e., 45 km). We suggest that continental adakitic rocks are not necessarily linked to high-pressure processes and their use as an indicator of thickened/delaminated continental crust should be regarded with caution.",
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Generation of continental adakitic rocks : crystallization modeling with variable bulk partition coefficients. / Dai, Hong Kun; Zheng, Jianping; Zhou, Xiang; Griffin, W. L.

In: Lithos, Vol. 272-273, 02.2017, p. 222-231.

Research output: Contribution to journalArticleResearchpeer-review

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