Brief introduction of Xishuangbanna, Yunnan

Xishuangbanna Dai Autonomous Prefecture is one of the eight autonomous prefectures in Yunnan Province and the capital of Jinghong City. Located at the southernmost tip of Yunnan Province, it is located at about 2 1 10' north latitude and 99 55' east longitude to 10 1 50' east longitude. It belongs to the tropical humid area south of the Tropic of Cancer, and is connected with Jiangcheng County and Pu 'er City in the east and west. It borders Lancang County in the northwest, Laos, Myanmar in the southeast, Myanmar in the south and Vietnam in the southwest. The length of the border line is 966.3 kilometers, which is about equal to 1/4 of the total length of the border line in Yunnan Province, with an area of 19582.45 square kilometers.

Xishuangbanna is located on the northern edge of tropical zone and belongs to the climate of tropical monsoon forest. As of 20 17, Xishuangbanna has administered 1 county-level cities and 2 counties. In 20 17, the total resident population of Xishuangbanna was1180,000, of which the minority population was 778,700, with the Dai as the main ethnic group, and 13 ethnic groups lived in the world. In 20 17, Xishuangbanna's GDP was 39,384.37 billion yuan, the per capita disposable income of urban residents was 2720 1 yuan, and the per capita disposable income of rural residents was 12043 yuan.

Extended data:

geologic structure

Xishuangbanna is divided by Lancang River Fault, which spans Tanggula-Changdu-Lanping-Simao and Gongshan-Tengchong fold systems. The former is Banpo anticlinorium and Dehua syncline, and the latter is located at the southeast end of Lincang-Menghai fold system.

Banpo anticlinorium is dominated by Mesozoic flysch formation-like, intermediate-acidic and intermediate-basic volcanic formations, accompanied by molasses formations, with red formations exposed sporadically and Cenozoic molasses formations unconformity. Dehua syncline and Mesozoic red strata are widely distributed, some of which are molasse strata, carbonate strata and coal-bearing clastic rocks. The Proterozoic Lancang Group and Damenglong metamorphic rocks are exposed at the southeast end of Lincang-Menghai fold, and the granite basement of Menghai in Variscan-Indosinian period occupies a large space.

Baidu Encyclopedia-Xishuangbanna Dai Autonomous Prefecture