GEOCHRONOLOGY, GEOCHEMISTRY AND TECTONIC IMPLICATIONS OF XIONGSHAN DIABASIC DIKE SWARM, NORTHERN FUJIAN

Authors
REN SL LI JL ZHOU XH SUN M
Citation
Sl. Ren et al., GEOCHRONOLOGY, GEOCHEMISTRY AND TECTONIC IMPLICATIONS OF XIONGSHAN DIABASIC DIKE SWARM, NORTHERN FUJIAN, SCIENCE IN CHINA SERIES D-EARTH SCIENCES, 40(4), 1997, pp. 411-417
Citations number
12
Categorie Soggetti
Geosciences, Interdisciplinary
Journal title
SCIENCE IN CHINA SERIES D-EARTH SCIENCES → ACNP
ISSN journal
10069313
Volume
40
Issue
4
Year of publication
1997
Pages
411 - 417
Database
ISI
SICI code
1006-9313(1997)40:4<411:GGATIO>2.0.ZU;2-A
Abstract
Sm/Nd isotopic age determination showed that Xiongshan dike swarm was at 585.7 Ma +/- 30 Ma. The trace element geochemistry and Sr/Nd/Pb iso tope geochemistry studies indicate that the dike swarm was products of back-are basin spreading ridge and the magma originated from the depl eted mantle region which was metasomatized by LILE-rich liquids/melts derived from subduction slab.