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Geochronology, petrology and geochemistry of the Mesozoic Dashizhuzi granites and lamprophyre dykes in eastern Hebei – western Liaoning: implications for lithospheric evolution beneath the North China Craton

Published online by Cambridge University Press:  05 June 2017

LE XIONG ,
JUNHAO WEI ,
WENJIE SHI ,
LEBING FU ,
HUAN LI ,
HONGZHI ZHOU ,
JIAJIE CHEN  and
MENGTING CHEN
LE XIONG*
Affiliation:
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
JUNHAO WEI
Affiliation:
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
WENJIE SHI
Affiliation:
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
LEBING FU
Affiliation:
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
HUAN LI
Affiliation:
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
HONGZHI ZHOU
Affiliation:
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
JIAJIE CHEN
Affiliation:
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
MENGTING CHEN
Affiliation:
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
*
*Author for correspondence: [email protected]
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Abstract

Geochronological, elemental and isotopic data of the Dashizhuzi granites and lamprophyre dykes from the eastern Hebei – western Liaoning on the northern North China Craton (NCC) provide an insight into the nature of their magma sources and subcontinental lithospheric mantle. The Dashizhuzi granites have an emplacement age of 226 Ma. They have enriched lithospheric mantle type 1 (EM1-like) Sr–Nd isotopic compositions, and have distinctive features of high Na2O and Sr and low Y with high Sr/Y and (La/Yb)N ratios. These characteristics show that the Dashizhuzi granites originated directly from melting of mafic lower crust composed of pre-existing ancient crustal and enriched mantle-derived juvenile crustal materials at normal continental crustal depth of 33–40 km. The lamprophyre dykes are dated at 167 Ma, and can be divided into two groups. The Group 1 dykes have variable Sr–Nd isotopic compositions and mid-ocean-ridge basalt (MORB-) like Th/U, Ba/Th and Ce/Pb ratios, whereas the Group 2 dykes have enriched Sr–Nd isotopic compositions and notable high Co, Cr, MgO and low Al2O3 characteristics. These distinctive features suggest that the Group 1 dykes were derived from a relatively fertile lithospheric mantle source (garnet-facies amphibole-bearing lherzolite) which has experienced variable degrees of asthenospheric mantle-derived melt–peridotite interaction prior to melting. However, the Group 2 dykes were derived from an ancient garnet-facies phlogopite and/or amphibole-bearing lherzolite lithospheric mantle. Thinning of the Early Mesozoic lithospheric mantle beneath the northern NCC is dominantly through melt–peridotite interaction and thermo-mechanical erosion prior to Middle Jurassic time. The chemical compositions have been modified at the bottom of the lithospheric mantle through melt–peridotite interaction processes.

Keywords

mafic dykeadakitic rocksMesozoic periodlithospheric thinningYanshan fold belt
Type
Original Article
Information
Geological Magazine , Volume 155 , Issue 7 , October 2018 , pp. 1542 - 1565
Copyright
Copyright © Cambridge University Press 2017 

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