By Li, Chun-Feng; Li, Qianyu; Wang, Pinxian
ISBN-10: 0444593888
ISBN-13: 9780444593887
Geology of the China Seas represents the 1st English-language synthesis of the on hand study into the geology of the South and East China Seas. one of the marginal basins around the globe, those components were the focal point of intensive study actions within the final 3 a long time, and at the moment are one of the international sizzling spots in hydrocarbon explorations and clinical investigations. The area is experiencing swift fiscal improvement with the offshore petroleum offering nearly one 3rd of the household hydrocarbon creation for mainland China. gasoline hydrates were effectively recovered from the China Seas for the 1st time.
Over the years, many volumes at the geology of the China Seas were released in chinese language. even supposing progressively more papers in English have seemed lately, the bulk care for neighborhood or local paleo-environment and sedimentology, and are scattered in numerous journals. This booklet brings jointly this wealthy facts in a single source, fairly that generated via chinese language marine geologists and petroleum geologists, and offers the first actual synthesis of the geology off China.
- The first systematic precis of the geology of the China Seas
- Includes entire insurance of the South China Sea and the East China Sea, together with the Yellow Sea and Bohai Gulf
- Reviews 1000s of chinese language guides on marine and petroleum geology now not at the moment available to the overseas community
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Extra resources for Geology of the China Seas
Example text
Since the 1990s, a number of paleomonsoon cruises to the SCS were organized, leading to numerous research projects mostly on variability and evolution of the East Asian monsoon over the Quaternary. Meanwhile, the modern monsoon studies have revealed complicated relations between monsoon intensity and spatial variations in precipitation. For example, the “South China Sea Monsoon Experiment (SCSMEX)” from 1996 to 2001 found that a strong (weak) monsoon over the SCS often leads to lesser (more) precipitation over the middle and lower reaches of the Yangtze River Basin and more (lesser) precipitation in North China (Ding, Li, & Liu, 2004).
Flows along the western boundary in the southern SCS, apparently veering eastward off central Vietnam near 12 N (Wang, Chen, & Su, 2006). 8 m/s and plays a significant role in the SCS oceanography by dividing it into the northern and southern parts. , 2006). Along with the major gyres, other specific features of the SCS surface circulation have been observed. The South China Sea Warm Current, for example, is a northeastward counterwind current in winter occurring off the Guangdong coast in the NE part of the SCS.
The Indian and western North Pacific summer monsoons, including the SCS monsoon, are of tropical nature in which the low-level winds reverse from winter easterlies to summer westerlies, but the East Asian summer monsoon is a subtropical structure in which the low-level winds reverse primarily from winter northerlies to summer southerlies (Wang & Lin, 2002). This definition does not fully agree with the conventional view of Chinese meteorologists, who usually embraces the SCS in the East Asian monsoon region together with the ECS.
Geology of the China Seas by Li, Chun-Feng; Li, Qianyu; Wang, Pinxian
by Steven
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