Chinatown Gangs: Extortion, Enterprise, and Ethnicity by Ko-lin Chin

By Ko-lin Chin

In Chinatown Gangs, Ko-lin Chin penetrates a closed society and provides a unprecedented portrait of the underworld of recent York City's Chinatown. in line with first-hand bills from gang participants, gang sufferers, neighborhood leaders, and legislation enforcement specialists, this pioneering research unearths the pervasiveness, the muscle, the toughness, and the institutionalization of Chinatown gangs. Chin finds the phobia gangs instill within the chinese language neighborhood. whilst, he indicates how the commercial viability of the group is sapped, and the way gangs inspire lawlessness, creating a mockery of legislation enforcement agencies.

Ko-lin Chin makes transparent that gang crime is inexorably associated with Chinatown's political economic climate and social historical past. He exhibits how gangs are shaped to turn into "equalizers" inside a social atmosphere the place person and team conflicts, even if social, political, or monetary, are not likely to be solved in American courts. additionally, Chin argues that Chinatown's casual economic climate presents another chance for road gangs to develop into "providers" or "protectors" of unlawful providers. those gangs, for this reason, are the pathological manifestation of a closed neighborhood, one whose difficulties aren't simply seen--and much less simply understood--by outsiders.

Chin's concrete facts on gang features, actions, equipment of operation and violence make him uniquely certified to suggest how you can restrain gang violence, and Chinatown Gangs closes together with his particular coverage feedback. it's the definitive examine of gangs in an American Chinatown.

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Additional info for Chinatown Gangs: Extortion, Enterprise, and Ethnicity (Studies in Crime and Public Policy)

Sample text

1, 12). Structures south of the Red River fault system in the Ailao Shan and the Lanping-Simao fold belt also appear to be distorted in the same sense. Assuming this is a structural bend, it records ~60–70 km of left-lateral shear (see Fig. 12). Some clockwise rotation on the western part of the Red River fault (see following paragraph) would reduce this offset by a few kilometers. The active Jianshui and Qujiang faults also curve in the same way, supporting the interpretation that this is a structural bend (see following paragraph).

Tectonic map of the Red River and Dali fault systems in western Yunnan. For location see Figure 3. a) The major faults of the Red River and Dali fault systems and the location of other figures. Inset in upper right shows the main tectonic units discussed in the text. Some faults of the Xianshuihe-Xiaojiang fault system are shown where they adjoin the Red River fault system. b) More detailed maps of the Red River fault and its relation to the rock units of the northeastern part of the Lanping-Simao unit in the Ailao Shan (lower left) and faults of the southeastern part of the Red River fault and adjacent Cenozoic rocks.

Right-slip faults associated with the Xiaojiang segment. Within the southern segment of the Xianshuihe-Xiaojiang fault system are numerous faults that lie between the main fault strands of the system but do not cut them. Most of these faults strike to the northeast and occur in the central part of the segment between Tonghai Lake and Dongchuan (Figs. 13, 21). They often follow old northeast-trending structural features, but in several places they offset rivers right-laterally, indicating that at least some of these faults are active and related to the Xianshuihe-Xiaojiang system (Plate 24).

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