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(1997)
The upper mantle activation in South China Sea and the lndosinian mantle plume
(1996)
Ttctonostratigraphic t e m e s and detachment
Taylor Taylor, Hayes Hayes (1983)
Origin and history of the South China Sea basinThe Tectonic and Geologic Evolution of Southeast Asian Seas and Islands. Part 2. Geophys. Monogr, 27
(1990)
The geology of Philippine Sea
R. Hall, J. Ali, Charles Anderson, Simon Baker (1995)
Origin and motion history of the Philippine Sea PlateTectonophysics, 251
(1990)
South-cast Asian Marginal Basins (South
(1996)
Ttctono - stratigraphic t e m e s and detachment faulting of the South China Sea and Sulu S e a Marine Geology
(1958)
Born in 1958; graduated from the Geological College of East China and completed
(1993)
Lithosphcrc structure and dynamics
C. Pigram, P. Symonds (1991)
A review of the timing of the major tectonic events in the New Guinea OrogenJournal of Southeast Asian Earth Sciences, 6
(1991)
The geological memoir of South China Sea
(1970)
Gunung Kinabalu
C. Rangin, J. Stephan, C. Müller (1985)
Middle Oligocene oceanic crust of South China Sea jammed into Mindoro collision zone (Philippines)Geology, 13
T. Lee, L. Lawver (1995)
Cenozoic plate reconstruction of Southeast AsiaTectonophysics, 251
A. Richardson (1993)
Lithosphere structure and dynamics of the Banda Arc collision zone, Eastern Indonesia, 33
(1991)
A review of the timing
the Banda Arc collision zone
D. Clague, R. Jarrard (1973)
Tertiary Pacific Plate Motion Deduced from the Hawaiian-Emperor ChainGeological Society of America Bulletin, 84
(1990)
Sulu and Celebes Seas): New data and interpretations
Continental laycr-controlled tectonics introduction
(1991)
Basic features and evolutional process of dispersed block of Meso - Cenozoic South China continental margin
H. Schlüter, K. Hinz, M. Block (1996)
Tectono-stratigraphic terranes and detachment faulting of the South China Sea and Sulu SeaMarine Geology, 130
Di Zhou, Ke Ru, Han-zong Chen (1995)
Kinematics of Cenozoic extension on the South China Sea continental margin and its implications for the tectonic evolution of the regionTectonophysics, 251
(1992)
Geologic-Gcophysic Features of China Seas and Adjacent Regions
(1990)
South - cast Asian Marginal Basins ( South China , Sulu and Celebes Seas ) : New data and interpretations
R. Hall, G. Nichols (1990)
Terrane amalgamation in the Philippine Sea marginTectonophysics, 181
(1995)
Cenozoic plate reconstruction of southeast
Jacobson (1970)
Gunung Kinabalu, Sabah, MalaysiaGeol. Suru. Malaysia Rept., 8
(1993)
Lithosphcrc structure and dynamics of
(1991)
Studies on the layer slip-dip slip fault structures and the petroleum geology (Taking the Middle-lower Yangzi area as an example). A research monograph of the oil and natural gas (2)
(1998)
Basic characteristics of extension structure in northem Nansha Islands, China, and its dynamical implications
(1990)
Terrane amalgamation in the Philippine
R. Mccabe, S. Harder, J. Cole, E. Lumadyo (1993)
The Use of Paleomagnetic Studies in Understanding the Complex Tertiary Tectonic History of East and Southeast AsiaJournal of Southeast Asian Earth Sciences, 8
(1997)
Physical modelling of plastic-flow network and multi-layer tectoinc deformation in the lithosphere
(1983)
The Tectonic and Geologic Evolution of Southeast Asian Seas and Islandr, Geophysical Monograph
(1983)
On the formation and evolution of the Mesozoic - Cenozoic active continental margin and island arc tectoincs of the western Pacific Ocean
S. Murauchi, W. Ludwig, N. Den, H. Hotta, T. Asanuma, T. Yoshii, A. Kubotera, K. Hagiwara (1973)
Structure of the Sulu Sea and the Celebes SeaJournal of Geophysical Research, 78
(1993)
Lithosphcrc structure and dynamics of 78 ( 17 ) : 3437 - 3447 . the Banda Arc collision zone , Eastern Indonesia Gml
Y. Okubo, T. Ishihara, M. Daigo (1997)
Magnetic anomalies of east and southeast Asia andtheir linear featuresJournal of Asian Earth Sciences, 15
Abstract The Nansha ultra‐crust layer‐block is confined by ultra‐crustal boundary faults of distinctive features, bordering the Kangtai‐Shuangzi‐Xiongnan extensional faulted zone on the north, the Baxian‐Baram‐Yoca‐Cuyo nappe faulted zone on the south, the Wan'an‐Natuna strike‐slip tensional faulted zone on the west and the Mondoro‐Panay strike‐slip compressive faulted zone on the east. These faults take the top of the Nansha asthenosphere as their common detachmental surface. The Cenozoic dynamic process of the ultra‐crust layer‐block can be divided into four stages: K2‐E21, during which the northern boundary faults extended, this ultra‐crust layer‐block was separated from the South China‐Indosinian continental margin, the Palaeo‐South China Sea subducted southwards and the Sibu accretion wedge was formed; E22‐E31, during which the Southwest sub‐sea basin extended and orogeny was active due to the collision of the Sibu accretion wedge; E32‐N11, during which the central sub‐sea basin extended, the Miri accretion wedge was formed and “A‐type” subduction of the southern margin of the north Balawan occurred; N12‐the present, during which large‐scale thrusting and napping of the boundary faults in the south and mountain‐building have taken place and the South China Sea stopped its extension.
Acta Geologica Sinica (English Edition) – Wiley
Published: Dec 1, 1999
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