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This volume is an extended Proceedings of the ''Ophiolite Symposium'' which was held during the 29th International Geological Congress, Kyoto, Japan, 24 August--3 September, 1992. If focuses on the multiplicity and diversity of the circum-Pacific Phanerozoic ophiolites and their intra-continental analogues. An introductory paper, summarizing characteristics of the circum-Pacific ophiolites is followed by papers dealing with particular segments of circum-Pacific ophiolite belts arranged in a counter-clockwise direction from New Zealand to Japan. These are followed by comprehensive documentations on multiple ophiolite belts within the Asian continent, as well as by a paper on a Tethyan ophiolite in Iran. Additionally, a report and a general view on the Late Proterozoic ophiolites are included.
Collision between Australia and SE Asia began in the Early Miocene and reduced the former wide ocean between them to a complex passage which connects the Pacific and Indian Oceans. Today, the Indonesian Throughflow passes through this gateway and plays an important role in global thermohaline flow. The surrounding region contains the maximum global diversity for many marine and terrestrial organisms. Reconstruction of this geologically complex region is essential for understanding its role in oceanic and atmospheric circulation, climate impacts, and the origin of its biodiversity. The papers in this volume discuss the Palaeozoic to Cenozoic geological background to Australia and SE Asia collision. They provide the background for accounts of the modern Indonesian Throughflow and oceanographic changes since the Neogene, and consider aspects of the region's climate history--
The Lapita Cultural Complex--first uncovered in the mid-20th century as a widespread archaeological complex spanning both Melanesia and Western Polynesia--has subsequently become recognized as of fundamental importance to Oceanic prehistory. Notable for its highly distinctive, elaborate, dentate-stamped pottery, Lapita sites date to between 3500-2700 BP, spanning the geographic range from the Bismarck Archipelago to Tonga and Samoa. The Lapita culture has been interpreted as the archaeological manifestation of a diaspora of Austronesian-speaking people (specifically of Proto-Oceanic language) who rapidly expanded from Near Oceania (the New Guinea-Bismarcks region) into Remote Oceania, where no humans had previously ventured. Lapita is thus a foundational culture throughout much of the southwestern Pacific, ancestral to much of the later, ethnographically-attested cultural diversity of the region.