Travel time of accreted igneous assemblages in western Pacific orogenic belts and their associated sedimentary rocks
Accreted igneous assemblages in orogenic belts maybe divided into three types depending on whether they derive from seamounts, ocean ridges or subduction-related ophiolites. Seamount type basalts are associated with shallow water sediments—mostly reefoidal limestones. Ocean ridge type basalts are ge...
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Veröffentlicht in: | Tectonophysics 2004-11, Vol.393 (1), p.241-261 |
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