The tension movement of the Okinawa Trough

Lin Changsong; Wang Ying

Volume 21 Issue 5

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Lin Changsong, Wang Ying. The tension movement of the Okinawa Trough[J]. Haiyang Xuebao, 1999, 21(5): 95-100.

Citation:

Lin Changsong, Wang Ying. The tension movement of the Okinawa Trough[J]. Haiyang Xuebao, 1999, 21(5): 95-100.

Lin Changsong, Wang Ying. The tension movement of the Okinawa Trough[J]. Haiyang Xuebao, 1999, 21(5): 95-100.

Citation:

Lin Changsong, Wang Ying. The tension movement of the Okinawa Trough[J]. Haiyang Xuebao, 1999, 21(5): 95-100.

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The tension movement of the Okinawa Trough

Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012

Received Date: 1997-11-05
Rev Recd Date: 1999-04-05

Abstract

Abstract

The tilt movement of the Ryukyu island-arc system toward the ocean trench and the waving movement of the mantle stream in the island-arc-back-arc area are the power source of the movement of the Okinawa Trough,The Okinawa Trough is a negative structure under the tension field after Tertiary,Modern trough inherits the old trough and develops in its staged style.From Later Miocene,the increase of tension movement of the Okinawa Trough is deeply related to the increment of subduction movement of the Philippine Sea Plate,but this movement cannot cause a large-scale spreading.
- Tension movement,
- waving movement,
- tilt movement

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References(23)

References

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