作者: D. P. MCKENZIE
DOI: 10.1038/226239A0
关键词: Hellenic arc 、 Convergent boundary 、 Feature (archaeology) 、 Plate tectonics 、 Oceanic basin 、 Mediterranean climate 、 Induced seismicity 、 Paleontology 、 Geology 、 Eastern mediterranean
摘要: The seismicity and fault plane solutions in the Mediterranean area show that two small rapidly moving plates exist Eastern Mediterranean, such may be a common feature of contracting ocean basins. results concepts plate tectonics apply to instantaneous motions across continental boundaries.