ISBN-10: 0875905005
ISBN-13: 9780875905006
ISBN-10: 1118670361
ISBN-13: 9781118670361
About The Product
Published via the yankee Geophysical Union as a part of the Geodynamics Series.
The contributions to this quantity were equipped into different types: common stories, which take care of the dynamic techniques, and the systematic geological and geophysical relationships of significance to the area as a complete; and nearby reviews, which specialise in particular components and contours of the Western Pacific. The composition of the quantity displays the learn efforts undertaken within the Western Pacific in the framework of the Geodynamics venture, via the international locations of the quarter and by means of different international locations focused on the geodynamics of the Western Pacific. the recent figuring out of the dynamics and improvement of the trench-arc-backarc structures, and the dynamic courting of the Western Pacific basin lithosphere and historic continental margins with trench-arc-backarc improvement, led to throughout the Geodynamics undertaking, is a big development within the geosciences. a lot of those new findings is contained during this quantity. The editors desire to thank all the authors for his or her remarkable contributions, and for his or her endurance with the enhancing approach and meeting of the booklet.
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Additional info for Geodynamics of the Western Pacific-Indonesian Region
Sample text
8). , the Ryukyus beneath the axis of the Nankai Trough. This pattern of seismicity along the Nankai Trough is quite different and Luzon Straits. 6). the other subduction zones in the western Pacific region. 5 earthquakes, explain this anomalously strong coupling between the plates. In the overriding plate, large earthquakes died by Wu (1970, 1978), Sudo (1972b), and Seno and Kurita (1978). 5)have occurred infrequenUy on the Japan Sea mode of rupture is: strike-slip faulting with P-axis trending nearly east-west off the eastern coast of have been stu- coast.
5 em/yr rate alongSaga• and Nankai Troughs. For the models which do not use the seis•e slip vectors along the Izu-Mariana-Yap are as the data, those slip vectors, aRhough only a few in number, e• be used in testing the convergence vector along this are section. However, the back-are spreading in the Mariana Trough and [he possible existence of the Caroline plate make a •reet comparison questionable. Both of the convergence vectors of FiLeh's (197a) and of the deviations determination seem to be of the focal solubions.
He trend of the are. Eguehi (19B1) interpreted this event as left-lateral strike-slip faulting on a transform fault which offsets the spreading center. , 197B). At the Yap Caroline Ridge, strike-slip type part and aL the Trench, a large buoyant mass, the is colliding •4th the trench. lEO and 119). la0) contain• considerable portion t•hese solutions. cal data, Weissel and Anderson (i97B) proposed the existence of a Caroline plate, deeoupled from the Pacific plate •o the east of the Yap-Palau Trench.
Geodynamics of the Western Pacific-Indonesian Region
by Ronald
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