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- Publisher
- Springer Journals
- Copyright
- Copyright © Science in China Press 2005
- Subject
- Geosciences; Geosciences, general
- ISSN
- 1674-7313
- eISSN
- 1862-2801
- DOI
- 10.1360/04yd0341
- Publisher site
- See Article on Publisher Site
Abstract
A belt of low Al-Trondhjemite-Tonalite-Diorite (TTD) series has been recognized along the Northern Qinling Orogenic Belt (NQOB), which is dated as 430―399 Ma and characteristic of positive εNd(t) values. Geochemical features and trace elements simulation indicate that the TTD series was probably originated from differently partial melting of tholeiitic rocks from the Erlangping group. Thermodynamic analysis on the residue phases of the partial melting processes suggests that the TTD series may represent a dynamic process of temperature-increasing and pressure-decreasing, indicating an extension and thinning process of a thickened crust.
Journal
Science China Earth Sciences – Springer Journals
Published: Nov 1, 2005
Keywords: Northern Qinling; Caledonian movement; Erlangping group; TTD series; trace elements simulation; partial melting; isotopic dating; experimental petrology