Protracted oceanic subduction prior to continental subduction: New Lu-Hf and Sm-Nd geochronology of oceanic-type high-pressure eclogite in the western Dabie orogen

Hao Cheng, S. Andrew DuFrane, Jeffrey D. Vervoort, Eizou Nakamura, Yong Fei Zheng, Zuyi Zhou

Research output: Contribution to journalArticle

32 Citations (Scopus)

Abstract

Oceanic-type high-pressure eclogite from the Huwan mélange in the western partof the Dabie orogen, north of the classic ultrahigh-pressure terrane, has been investigated with combined Lu-Hf and Sm-Nd geochronology. The eclogites are thought to have formedduring the subduction of oceanic crust prior to the subduction of the Yangtze craton beneath the North China block. Garnet Lu-Hf and Sm-Nd garnet-whole rock dates yield similar ages of 257.4 ± 1.4 and 252.5 ± 2.7 Ma, the youngest ages reported thus far fromthis mélange. Despite the partially preserved prograde major- and trace-element zoning in garnets, the Lu-Hf and Sm-Nd ages mostly reflect the high-pressure eclogite-facies metamorphism instead of the early phase of garnet growth. The data define a new high-pressure age population for the Dabie orogen, which provides a more detailed insight intothe subduction history of the Yangtze craton before continental collision. The new Lu-Hf and Sm-Nd dates for these oceanic-type eclogites, combined with existing geochronologicalinformation, range from 315 to 253 Ma. This broad interval suggests that the overall subduction of oceanic crust occurred over a period of ∼60 Ma and that different slices withdistinct pressure-temperature histories underwent HP metamorphism at distinct times. Amodel of a continuous evolution from oceanic to continental subduction is favored, and the onset of the deeply continental subduction occurred probably not before ca. 257 Ma.

Original languageEnglish
Pages (from-to)1214-1223
Number of pages10
JournalAmerican Mineralogist
Volume95
Issue number8-9
DOIs
Publication statusPublished - Aug 2010

Fingerprint

Geochronology
geochronology
eclogite
Garnets
subduction
garnets
garnet
cratons
oceanic crust
craton
crusts
metamorphism
Zoning
histories
Trace Elements
continental collision
history
trace elements
zoning
Rocks

Keywords

  • Dabie
  • Eclogite
  • Lu-Hf
  • Oceanic subduction
  • Sm-Nd

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

Protracted oceanic subduction prior to continental subduction : New Lu-Hf and Sm-Nd geochronology of oceanic-type high-pressure eclogite in the western Dabie orogen. / Cheng, Hao; DuFrane, S. Andrew; Vervoort, Jeffrey D.; Nakamura, Eizou; Zheng, Yong Fei; Zhou, Zuyi.

In: American Mineralogist, Vol. 95, No. 8-9, 08.2010, p. 1214-1223.

Research output: Contribution to journalArticle

Cheng, Hao ; DuFrane, S. Andrew ; Vervoort, Jeffrey D. ; Nakamura, Eizou ; Zheng, Yong Fei ; Zhou, Zuyi. / Protracted oceanic subduction prior to continental subduction : New Lu-Hf and Sm-Nd geochronology of oceanic-type high-pressure eclogite in the western Dabie orogen. In: American Mineralogist. 2010 ; Vol. 95, No. 8-9. pp. 1214-1223.
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