Xinjiang county, Yuncheng City, Shanxi Province

Xinjiang county, subordinate to Yuncheng City, Shanxi Province, is located in the southwest of Shanxi Province, with a total area of 597.18 square kilometers, belonging to warm temperate continental climate. Xinjiang county governs nine towns and two township level units. The county government is located in Longxing town. By the end of 2018, the number of permanent residents in Xinjiang county was 347891.

In the second year of Wucheng (560), the Ming emperor of the Northern Zhou Dynasty changed Dongyong Prefecture into Jiangzhou and moved to Longtou city of Wenxi County (today's Longtou fort in Liyuan Town). In 2001, Yuncheng City was built from land. Xinjiang county is under the jurisdiction of Yuncheng City. Xinjiang Daxi passenger dedicated line passes through the eastern edge. Beijing Kunming expressway, Linghou Expressway and Houping Expressway meet in the territory. Houxi railway, 108 National Highway Cross East and West, 232 provincial highway cross north and south. Xinjiang county has Longxing Temple, Ji Yi temple, Jiang Zhou Town God's Temple and other scenic spots. In March 2019, it will be listed in the first batch of counties for the protection and utilization of revolutionary cultural relics.

In 2018, the GDP of Xinjiang county was 9812.34 million yuan, which was 10.1% higher than that of 2017 at comparable prices. Among them, the added value of the primary industry was 1822.14 million yuan, an increase of 3.2%; the added value of the secondary industry was 4617.01 million yuan, an increase of 12.8%; the added value of the tertiary industry was 3373.19 million yuan, an increase of 10.9%.

Historical evolution

During the Western Zhou Dynasty, King Wu granted the 17th son of King Wen the Marquis of Ying, who ruled the Xinjiang region. Later, he changed the Marquis of Ying to Xun and became the Marquis state. In the spring and Autumn period, the state of Xun was destroyed by Jin, which belonged to Jin. In 668 BC, Jin Xiangong moved his capital to gujiang (now Jincheng, North Xiangfen County, Xinjiang). In 585 BC, Jin Jinggong moved his capital to Xintian (now hengqiao township of Xinjiang county), which is known as Xinjiang in history. Three kilometers to the south of the county, there used to be Jueqi palace, the Royal Palace of Jin State. This is dongshengzhuang. There is jinjiangxiao building (linggongtai) in Zezhang Town, northwest of the county. It is said in history that "Duke Ling of Jin Dynasty is not the king, but he hits people with bullets. That's it.

During the Warring States period, Han, Zhao and Wei were divided into three families, which belonged to Wei, called Fencheng, and belonged to Hedong county.

Qin still belongs to Hedong county. Linfen County in the north and Changxiu County in the West. The old city of Linfen is 25 kilometers north of the present county (Jincheng village, Xiangfen County). Changxiu ancient city is 15 kilometers northwest of the present county (Quanzhang Town, Xinjiang county).

During the reign of emperor Gaozu of the Han Dynasty, Du Tian was granted the title of Marquis of Changxiu and the Marquis of Changxiu. In the Eastern Han Dynasty, it was changed into Changxiu town.

Three Kingdoms belong to Wei, set Linfen County, Li Pingyang County.

In the Western Jin Dynasty, Linfen County belonged to Pingyang County.

In the northern and Southern Dynasties, in 427, Emperor Taiwu of the Northern Wei Dynasty set up dongyongzhou in Baibi town. Linfen county is divided into Taiping County and South Taiping County. Taihe 11 years (487) set Zhengping County, leading Wenxi, Quwo two counties. In the second year of Wucheng (560), the Ming emperor of the Northern Zhou Dynasty changed Dongyong Prefecture into Jiangzhou and moved to Longtou city of Wenxi County (today's Longtou fort in Liyuan Town). In the reign of Emperor Wu, he moved back to Baibi. In 577, he moved to Yubi, Jishan county.

Sui kaihuang three years (583 years) Zhou Zhi moved from Yubi to this county. Zhengping county was abolished and changed into Jiang county. Lingzhengping (now Xinjiang), Longmen, Taiping, Quwo, Yicheng, Jishan, Jiang and Yuanqu.

In 618, the first year of Wude of Tang Dynasty, Jiangzhou general manager's office was set up. Jurisdiction Jiang, Lu, Gai, Jian, Ze, Qin, Han, Jin, Lu, Hui, Qin, PU, Yu, Rui, Shao and other 15 states. Jiangzhou led Zhengping, Taiping, Quwo, Wenxi and Jishan counties. In the third year of Wude (620), the general manager's office was dismissed and the county became the most powerful. Lingzhengping, Yicheng, Quwo, Wenxi, Yuanqu, Taiping and Jiang counties. In Zhenguan, Jiangzhou belongs to Hedong road. The rule is still the same.

The Five Dynasties inherited the Tang system.

Song Dynasty was the Xiongzhou, and set Jiangjun for defense. It has jurisdiction over seven counties, including Zhengping, Quwo, Yicheng, Taiping, Jishan, Jiang and Yuanqu.

Jinzhi Jiangyang army Jiedushi. Xingding two years (1218) was promoted to Jin'an house, the general manager of the South Road army. In the third year of Xingding (1219), the transportation department of hedongnan road was set up, leading eight counties, including Zhengping, Yicheng, Quwo, Wenxi, Yuanqu, Taiping, Jiang and Pingshui.

At the beginning of the Yuan Dynasty, it was Zhongzhou, where Jiangzhou was set up as marshal's mansion, which governed the counties of Hezhou and Jiezhou. After that, it was still Jiangzhou, attached to Pingyang Road, and led seven counties, including Zhengping, Yicheng, Quwo, Wenxi, Yuanqu, Taiping and Jiang.

In the Ming Dynasty, it was Jiangzhou, belonging to the Chief Secretary of Shanxi Province. It was subordinate to Pingyang Prefecture and led to three counties, namely Jishan, Yuanqu and Jiang.

At the beginning of the Qing Dynasty, it was still a leader. In the second year of Yongzheng reign (1724), it was changed into Jiangzhou, Zhili, with five counties including Jishan, Hejin, Wenxi, Yuanqu and Jiangzhou.

In May 1912, the first year of the Republic of China (1912), the state was abolished and the county was changed. Taking the meaning of "Xian" and "restoration", it was also different from the neighboring Jiang County, and then it was renamed "Xin Jiang county", which belongs to Hedong Road. In 1927, Dao was abolished and Zhili provincial government was established. In 1937, Xinjiang county belonged to the ninth Office of Shanxi Province. In 1939, the county government of the Republic of China moved to Xiachuan village, Xiangning County, and moved back in 1945. The puppet county government was still in the old city. In May 1945, the Anti Japanese democratic government of Xinjiang county was established in Wenhou village. In August of the same year, it was renamed as the democratic government of Xinjiang county. It was still stationed in Wenhou village and had jurisdiction over Wenxi Beiyuan 28 village. In April 1947, Xinjiang county was liberated and the people's Government of Xinjiang county was established. In the autumn of this year, Fenhe River was the boundary, and Jiangnan county was the south. It belonged to the third special office of Taiyue, and was stationed in Wenhou village. It still governed the area of Wenxi Beiyuan. In the north is Xinjiang county, which belongs to the Tenth Special Office of Luliang in Jinsui. In August 1948, Jiangnan county was incorporated into Xinjiang county, which is also the Tenth Special Office of Luliang in Jinsui. Both the special office and the county government are located in the present county. In February 1949, Jinnan administrative office was established in Xinjiang with three divisions. Xinjiang has jurisdiction over seven counties, including Xinjiang, Jishan, Hejin, Quwo, Xiangning, Jixian and Fencheng. In June of the same year, the Jinnan special office was established (in today's Linfen City), and Xinjiang belongs to the Jinnan special office.

At the end of 1949, Yuncheng special office was set up, and Xinjiang belongs to Yuncheng special office.

In November 1958, Xinjiang was incorporated into Houma City, belonging to Jinnan special office. In November 1961, it was separated from Houma City and resumed the establishment of Xinjiang county, which still belongs to Jinnan special office.

In 1970, Jinnan was divided into Linfen and Yuncheng districts, and Xinjiang was divided into Yuncheng district.

In 1979, Yuncheng district was renamed Yuncheng administrative Commissioner's office, and Xinjiang is still one of the counties under its jurisdiction.

In 2001, Yuncheng City was built from land. Xinjiang county is under the jurisdiction of Yuncheng City.

administrative division

As of December 2019, Xinjiang county has jurisdiction over nine towns: Longxing Town, Sanquan Town, Zezhang Town, Beizhang Town, Gujiao Town, Wan'an Town, yangwang Town, Quanzhang town and hengqiao town; another two township level units: Xinjiang community and Xinjiang Economic and Technological Development Zone. The county government is located in Longxing town.

geographical environment

Location context

Xinjiang county is located in the southwest of Shanxi Province, adjacent to Houma City in the East, Jishan County in the west, Wenxi County in the south, Xiangfen County in the northeast and Xiangning County in the northwest, with a total area of 597.18 square kilometers.

geology

stratum

Xinjiang county is located in the south of Shanxi platform. The exposed strata have the characteristics of Sino Korean platform, including Archean, Proterozoic, Paleozoic and Cenozoic.

Archean Archean strata are the oldest metamorphic rock series in the county, which are exposed in the northern Luliang Mountain Area and the southern yangjiayuan Beigou area. The exposed thickness is 200-1000m. The lithology is granite gneiss and hornblende plagioclase gneiss. The mineral composition of granitic gneiss is flesh red potash feldspar, quartz, biotite, etc. Hornblende plagioclase gneiss is mainly composed of black green hornblende and light gray plagioclase, with phosphorite locally. Because it is covered by Quaternary loess, there is no bottom.

The Neoproterozoic and Neoproterozoic Sinian system is unconformably overlaid on the pre Sinian gneiss in an angle, distributed in the Luliang Mountain area, with a thickness of 14 meters, and the lithology is gray white medium grained quartz sandstone.

The Cambrian of Paleozoic is parallel unconformity overlying the Sinian strata of Proterozoic. It is distributed in the Luliang Mountain area, with a thickness of 470 meters. It is marine shale and limestone. Ordovician strata are covered by Cambrian strata in parallel unconformity and exposed in Jiuyuan mountain and Luliang Mountain area. The thickness is about 430m, which is marine sedimentary dolomite and limestone. The Middle Carboniferous Benxi Formation consists of Shanxi type iron ore and iron sandstone, bauxite shale, black gray shale and gray white sandstone, which are parallel unconformity overlying Ordovician limestone. It is exposed at the junction of Lvliang mountain area and Xiangning County, with a thickness of about 20 meters.

The tertiary Pliocene strata of the Cenozoic are unconformably overlaid on the Archean granitic gneiss. The lower part is conglomerate and sandstone with a thickness of 80m. The upper part is purplish red Hippophae red soil, containing calcareous nodules, with a thickness of 22 meters, exposed in the area of yangjiayuan Beigou and Wenhou Donggou.

Quaternary strata in the territory of the deposition is very thick, because of the different location and sedimentary environment, lithology and thickness are different. The lower Pleistocene strata are not exposed in Xinjiang county and are all covered by the later strata. According to the drilling, the sedimentary thickness and lithology vary greatly, generally in the range of 50-188m. The Middle Pleistocene strata are exposed in emeiling, the gully wall of the third terrace and the scarp of the terrace, and are distributed in a strip shape. They are covered by the lower Pleistocene strata in parallel unconformity, and the upper part is covered by the upper Pleistocene strata. The lithology in the alluvial fan area is gravel, clay, clay and gravel interbedding. The genetic type is flood and slope. In the third stage area of Fenhe River, the lithology is composed of sub sandy soil, sub clay and sand interbedding, and the genetic type is flood and alluvial. In emeiling, the lithology is red and yellow clay, containing calcareous nodules and several layers of paleosol, which is flood and alluvial. The thickness is generally 46-19lm. The upper Pleistocene strata are widely distributed and exposed to the surface, with a thickness of 20-46m. In front of Luliang Mountain, the alluvial fan area is composed of pebble and pebble clay. stay