Where is Lake Sailimu? Which city?

Location of Sailimu Lake: Bole City, Bortala Region, Xinjiang.

Sailimu Lake is a provincial-level scenic spot and the fifth batch of national-level scenic spots. Sailimu Lake, called "Jinghai" in ancient times, is located in the northern Tianshan Mountains of Bole, Bortala Mongolian Autonomous Prefecture, Xinjiang, adjacent to Huocheng County, Ili Kazakh Autonomous Prefecture. The lake is 207 1 m above sea level, 30 kilometers long from east to west and 25 kilometers wide from north to south, covering an area of 453 square kilometers.

Sailimu Lake Scenic Area is divided into six functional areas: lake-surrounding scenic area, grassland nomadic customs area, ecological landscape protection area, swan and other rare bird habitat protection area, tourism comprehensive service area and original ecological environment protection area. Three special protected areas have been identified, namely, the central core water body of Sailimu Lake, the water body habitat of Swan Wetland Meadow in the West Sea and the ice and snow ecological exploration scenic spot in Chagan Guo Le.

Formation and evolution

According to the existing research data, the tectonic evolution of Sailimu Lake area can be summarized into three stages:

1, the assembling process of many ancient blocks before Sinian.

By Sinian, the main body began to form a unified craton block, and generally accepted the unified caprock deposits represented by Sinian moraine and early Cambrian phosphorus-bearing rock series.

2. The evolution process of early and middle Paleozoic splitting and recombination of Xinjiang plate.

From the Middle Cambrian to the end of the Late Carboniferous, the complex history of continental plate expansion, separation and subduction collision was completed, and finally the basic structural framework of Xinjiang was formed, ending the structural evolution stage of separation and combination of multi-plates and land in the early and middle Paleozoic. And entered the same plate, namely the stage of continental tectonic evolution.

3. Evolution stages of intracontinental structures in Xinjiang from Late Paleozoic to present.

At the end of Carboniferous and the beginning of Permian, the embryonic form of Eurasian plate was formed, and Xinjiang became a part of this global giant plate. However, on its south side, it is also faced with the closure of the Paleo-Tethys Ocean, the opening and final closure of the Neo-Tethys Ocean and the formation of the Qinghai-Tibet Plateau, which finally contributed to the tectonic subsidence lake-Sailimu Lake. ?

Reference to the above content: Baidu Encyclopedia-Sailimu Lake