Macquarie Home | Course Handbook | Library | Campus Map | Macquarie Contacts
Home page

Macquarie University ResearchOnline

Home
Add
-List Of Titles -Early J₂ basalts in SE China : incipience of large-scale late Mesozoic magmatism

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/35283

OpenURL Link
21 Visitors 22 Hits 0 Downloads
Title
Early J₂ basalts in SE China : incipience of large-scale late Mesozoic magmatism
Related
Science in China series D : earth sciences, Vol. 49, Issue 8, p.796-815
DOI
10.1007/s11430-006-0796-4
Publisher
Science in China Press
Date
2006
Author/Creator
Xie, Xin
Author/Creator
Xu, Xisheng
Author/Creator
Zou, Haibo
Author/Creator
Jiang, Shaoyong
Author/Creator
Zhang, Ming
Author/Creator
Qiu, Jiansheng
Description
Magmatism in SE China was dormant during 204–180 Ma, but was reactivated in 180–170 Ma (early J₂), and then became more and more intensive towards the end of early Cretaceous. The small-scale early J₂ magmatism is the incipience to long-term and large-scale magmatism in this region. A near east-west (EW) trend volcanic belt was distributed across south Hunan, south Jiangxi and southwest Fujian was formed during early J₂ time. Along this belt from the inland toward the coast, the lithology of basalts changes from alkali into tholeiite, and the amount of erupted volcanic rocks and the proportions of rhyolites coexisting with the basalts increase. On the basis of geochemical characteristics of these basalts, we infer that the melting degree of source rocks and the extent of fractional crystallization and crustal contamination all increased whereas the depth of mantle source decreased from the inland to the coast, which led to the variations of geological characteristics of the volcanic belt. In early J₂, the western spreading Pacific plate began to subduct underneath SE China continental block, reactivating near EW trend deep fault that was originally formed during the Indosinian event. The stress of the western spreading Pacific plate and the extent of asthenosphere upwelling increased from the inland to the coast, which is consistent with the generation and evolution of early J₂ basalts.
Description
20 page(s)
Subject Keyword
early J₂ basalts
Subject Keyword
upwelling of asthenosphere
Subject Keyword
large-scale magmatism
Subject Keyword
SE China
Subject Keyword
the Pacific plate
Resource Type
journal article
Organisation
Macquarie University. Dept. of Earth and Planetary Sciences

Identifier
http://hdl.handle.net/1959.14/35283
Identifier
ISSN:1862-2801
Identifier
mq-rm-2007011355
Language
eng
Reviewed
Reviewed
Save/E-mail Citation
Citation Format
E-mail Address
Subject
"Science in China series D : earth sciences"
 
OR
  • Show All  
  • Show My Selections 
Advanced Search

Search

Qiu, Jiansheng
Zhang, Ming

Browse

  • By Title 
  • By Author/Creator 
  • By Department/Centre 
  • By Subject Keyword 
  • By Journal/Conference 
  • By FoR/RFCD codes 
  • By Resource Type 
  • By Date 

Highlights

  • Most Accessed Objects 
  • Recent Additions 
  • Pending Publications 
  • Author Profiles 

Resources

  • About ResearchOnline 
  • FAQ 
  • Open Access 
  • Open Access-FAQs 
  • Copyright 
  • Contribute 
  • Help 
  • Contact
  • Terms and Conditions 
Valid XHTML 1.0 Strict Powered by VITAL

Copyright Macquarie University | Privacy Statement | Accessibility Information

ABN 90 952 801 237 | CRICOS Provider No 00002J

Library Staff Sign In