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The result of a conference cosponsored by the Sinological Institute, Leiden U., and the International Institute of Social History, Amsterdam, and held during January 1990, this collection of essays presents new perspectives on the history of the Chinese Communist Party (CCP) between its founding in 1920 and its conquest of China in 1949. Employing the voluminous primary sources that have become available in the last decade and a half, the authors draw attention to events and places that until now have suffered historiographical neglect or offer revisionist interpretations of the signal events and leading figures of CCP history, in many cases relating them to new theoretical perspectives on culture and local society, including language and gender relations. Paper edition (unseen), $32.50. Annotation copyright by Book News, Inc., Portland, OR
Permian and Triassic are the interval known for the integration and separation of Pangea, the closure of the Palaeotethys and the opening of Mesotethys. They were associated with a series of worldwide events including the Late Palaeozoic glaciation and succeeding extensive evaporatic and reef formations, the end-Palaeozoic regression, strong orogenies and widespread volcanism and magmatism, and finally, the Permo-Triassic biotic macro-extinction. These events resulted in the formation of enormous reserves of coal, petroleum, evaporites, phosphorites and metal resources. The Permian and Triassic thus constitutes a time interval particularly important both for understanding the Earth's history...
Geological Formation Names of China (1866—2000) is the only catalogue on stratigraphic nomenclature for China in the world to keep two writing types (Wade-Giles Romanization and Chinese Phonetic Alphabet) so as to provide convenience for domestic and overseas readers. The catalogue is intended for specialists and graduates in Geosciences and Stratigraphy. Shouxin Zhang (1927 —2006) was stratigrapher and research professor at the Institute of Geology and Geophysics, Chinese Academy of Sciences.
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Drawing on a wealth of new sources, this work documents the evolving relationship between Moscow and Peking in the twentieth century. Using newly available Russian and Chinese archival documents, memoirs written in the 1980s and 1990s, and interviews with high-ranking Soviet and Chinese eyewitnesses, the book provides the basis for a new interpretation of this relationship and a glimpse of previously unknown events that shaped the Sino-Soviet alliance. An appendix contains translated Chinese and Soviet documents - many of which are being published for the first time. The book focuses mainly on Communist China's relationship with Moscow after the conclusion of the treaty between the Soviet Un...
The ihsan Ketin NATO Advanced Study Institute on the Tectonic Evolution of the Tethyan Region was conceived in 1982 in Veszprem, Hungary, when three of the organizers (B. C. B. , L. H. R. and A. M. C. 9. ) had come together for a meeting on the tectonics of the Pannonian basin. All three of us had experience in the Tethyan belt and all three of us had been for some time deploring the lack of communication among workers of this immense orogenic belt. Much new work had been completed in such previously little-known areas as Turkey, Iran, Afghanistan, the People's Republic of China, the entire Himalayan region, as well as new work in the European parts of the chain. Also, ironically, parts of t...
The Permian was a remarkable time period. It represents the maximum stage of Pangean continental assembly, includes a major global climatic shift from glacial to nonglacial conditions (icehouse-greenhouse transition), and is ter minated by one of the most profound faunal/floral extinction events in the Earth's history. In addition, Permian oceans, although poorly understood, must have had some quite unique characteristics. Permian seas reached the most extreme values of carbon, sulfur, and strontium isotopic ratios ever achieved in Phanerozoic time, and the isotopic ratios of all three elements abruptly returned to more "normal" values at, or very close to, the Permo Triassic boundary. Final...