Journal
JOURNAL OF ASIAN EARTH SCIENCES
Volume 24, Issue 4, Pages 481-493Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.jseaes.2004.01.004
Keywords
paleomagnetism; vertical-axis rotation; extension; southeast China; Hong Kong
Categories
Ask authors/readers for more resources
A palcomagnetic study of Upper Cretaceous (similar to 80 Ma) dikes front Hong Kong was conducted with the aim of better understanding the Late Cretaceous-Cenozoic kinematic history of southeast China. Twelve out of seventeen sites collected from four dikes revealed primary TRMs and yield a Late Cretaceous paleopole at 69.3degreesN/211.2degreesE, where A(95) = 8.9degrees and K = 107. A synthesis of South China Block Cretaceous poles indicates that Coastal Southeast China, which is bounded by the Lianhuashan Fault Zone to the northwest and the Changle-Nanao Fault Zone to the southeast, has moved relative to inland Central South China. The discordant Cretaceous paleopoles from the South China Block suggest a moderate net clockwise rotation of the Coastal Southeast China relative to Central South China since the Late Cretaceous. This clockwise rotation is probably the result of micro-blocks along the South China margin experiencing vertical-axis rotations in response to the penetrative dextral shear along the SE China margin during oblique subduction of the Pacific Plate beneath South China. An alternative interpretation involves regional extension that displaced a raft-block southeastwards of the margin, generating apparent paleomagnetic records with no real block rotations. (C) 2004 Elsevier Ltd. All rights reserved.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available