Geologic Development of the Truong Son Fold Belt In Central Vietnam - Study on the Evolution of Asian Continent (IGCP-411) -
Geologic Development of the Truong Son Fold Belt In Central Vietnam - Study on the Evolution of Asian Continent (IGCP-411) -
批准号:
12573010
负责人:
HADA Shigeki
金额:
$4.16万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B)
财政年份:
2000
资助国家:
日本
项目状态:
已结题
起止时间:
2000 至 2002
中文摘要
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英文摘要
The purpose of this project is to clarify the tectonic evolution of Asian Continent that was formed by the complicated process started from the dispersion of Gondwanaland in the relation with the development of Japanese Islands. It is considered that the clarification of the tectonics of the orogenic belts in Vietnam is a key to this purpose. Japanese member of the project did the geological survey in the following areas by the assistance of Vietnam geologists; structural analysis and sampling of granitic rocks for age determination in the Son Ma Suture Zone, and sampling for paleomagnetic study in both sides of the Red River Fault (2000), sedimentary petrological study in the Truong Son Fold Belt and paleontological and structural study in northern Vietnam (2001), and tectonic analysis of the relationship between Indochina Block and adjacent blocks in Vietnam. The results of the geological survey are as follows; 1) Northern side of the red River Fault in Vietnam is divided into two bl … More ocks by the suture zone which is a southern extension from the South China Block. 2) Zone consisting of accretionary complex of ocean plate materials are recognized southern side of the Truong Son Fold Belt and its vergence is toward northeast. 3) Southeastern boundary of the Indochina Block does not exist inside Vietnam.Paleomagnetic, biostratigraphic and chronological, and sedimentary petrological studies are going on concerning samples collected from the areas mentioned above. Until now, the following points are made clear, 1) The corresponding poles in Cretaceous at two localities in the both sides of the Red River Fault are statistically indistinguishable from each other. 2) Accretionary Complex in the southern side of the Son Ma Suture Zone yields Devonian conodonts so that the continental fragment in the northern side of the Son Ma Suture Zone drifted from the Gondwanaland at least in Devonian. 3) Age of three granitic sample including plagiogranites (?) from the Son Ma Suture Zone is 238.9+/-1.8 Ma (Middle Triassic), 280.7+/-3.9 Ma (Early Permian) and 256.1+/-1.2 Ma (Middle Permian). 4) Suture zone between the Cathaysia and Yantze blocks in northeastern Vietnam is also contains Devonian conodonts. 4) On the basis of the sandstone petrography and geochemistry, the provenance in the Middle-Upper Paleozoic sequence in the Truong Son Fold Belt reveals the formation of the immature magmatic arc and distinct change of the provenance is considered as important scheme of Paleozoic tectonic development in northern Vietnam and adjacent terranes.From above-mentioned results of the study, we could indicate the following points at this stage. 1) The Truong Son Fold Belt is a suture zone between the Indochina and South China Continental Blocks. 2) Northern boundary of the Truong Son Suture Zone is the Son Ma Suture Zone and its southern boundary may be correspond to the Danang Fault. 3) Truong Son Suture Zone includes relicts of ocean-plate and island arc. 4) South China Continental Block in Vietnam is composed of Yantze and Cathaysia Blocks. Less
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Hada, S.: "Kurosegawa Terrane in Southwest Japan: Disrupted Remnants of a Gondwana-Derived Terranes"Gondwana research. 4 (1). 27-38 (2001)
Hada, S.:“日本西南部的黑濑川地体:冈瓦纳衍生地体的破坏遗迹”冈瓦纳研究。
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Shigeki HADA: "Kurosegawa Terrane in Southwest Japan : Disrupted remnants of a Gondwana-derived terrane"Gondwana Research. Vol.4,No.1. 27-38 (2001)
Shigeki HADA:“日本西南部的黑濑川地体:冈瓦纳大陆衍生地体的破坏遗迹”冈瓦纳研究。
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波田重煕: "ペルム紀紡錘虫類と黒瀬川地帯の起源"兵庫地学. No.46. 9-20 (2002)
Shigehiro Hata:“二叠纪纺锤体和黑濑河带的起源”兵库地质学No.46(2002)。
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Yang, Z.: "Discrepant Cretaceous paleomagnetic poles between Eastern China and Indochina: a consequence of extrusion of Indochina"Tectonophysics. 334. 101-113 (2001)
Yang, Z.:“中国东部和印度支那之间的白垩纪古地磁极差异:印度支那挤压的结果”构造物理学。
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Yang, Z.: "Discrepant Cretaceous paleomagnetic poles between Eastern China and Indochina : a consequence of the extrusion of Indochina"Tectonophysics. 334. 101-113 (2001)
Yang, Z.:“中国东部和印度支那之间白垩纪古地磁极的差异:印度支那挤压的结果”构造物理学。
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共 21 条
Basic Study on the Articulation of Curriculum between the Undergraduate Program and the Graduate Program.
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批准号:07451062
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项目类别:Grant-in-Aid for Scientific Research (B)
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资助金额:$0.77万
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财政年份:1995
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负责人:HADA Shigeki
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依托单位:
Physical and Mechanical Properties of the Tertiary Sedimentary Rocks in the Shimanto Belt in Shikoku.
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批准号:03640647
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项目类别:Grant-in-Aid for General Scientific Research (C)
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资助金额:$1.02万
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财政年份:1991
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负责人:HADA Shigeki
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依托单位:
"Usugimu-type conglomerate" and Processes of Collision and Accretion of the Kurosegawa Landmass
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批准号:63540611
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项目类别:Grant-in-Aid for General Scientific Research (C)
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资助金额:$0.83万
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财政年份:1988
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负责人:HADA Shigeki
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依托单位: