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Island arcs, deep sea trenches, and back-arc basins

種類:
電子ブック
責任表示:
edited by Manik Talwani and Walter C. Pitman III
出版情報:
1977
著者名:
シリーズ名:
Maurice Ewing series ; 1
ISBN:
9781118665756 [1118665759]  CiNii Books  Calil
注記:
Includes bibliographical references.
Some basic problems in the trench-arc-back arc system / Seiya Uyeda -- Subduction in the Indonesian region / Warren Hamilton -- Tectono-stratigraphic evolution of subduction-controlled sedimentary assemblages / William R. Dickinson -- Multifold seismic reflection records from the northern Venezuela Basin and the north slope of the Muertos Trench / John W. Ladd, J. Lamar Worzel, and Joel S. Watkins -- The initiation of trenches : a finite amplitude instability / D.P. McKenzie -- Lithospheric instabilities / D.L. Turcotte, W.F. Haxby, and J.R. Ockendon -- Mesozoic tectonics of the southern Alaska margin / J. Casey Moore and William Connelly -- Multi-channel seismic study in the Venezuelan basin and the Curaçao ridge / M. Talwani [and others] -- Geometry of Benioff zones : lateral segmentation and downwards bending of the subducted lithosphere / Bryan L. Isacks and Muawia Barazangi -- Bathymetric highs and development of convergent plate boundaries / John Kelleher and William McCann -- In situ P-wave velocities
Restrictions unspecified
Electronic reproduction. [S.l.] : HathiTrust Digital Library, 2010.
Master and use copy. Digital master created according to Benchmark for Faithful Digital Reproductions of Monographs and Serials, Version 1. Digital Library Federation, December 2002. http://purl.oclc.org/DLF/benchrepro0212
digitized 2010 HathiTrust Digital Library committed to preserve
Print version record.
Some basic problems related to thermo - mechanical aspects of trench -arc systems are discussed. The origin of high heat flow, volcanism and back arc basins, in particular, is considered from two basic models, i.e. the frictional heating model and the secondary mantle flow model. The possible effect of increasing subduction rate within the frictional model is considered also.
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