Can Chaoyang central hospital go to Wuzi

1. Hehe, you can go in after graation

do you want to go in without looking for someone? There's no door

2. It seems that hospitals can't shrink pores.
it's better to go to a bigger beauty salon. If there are 7-8 receptacles, they may be charged according to the number.
it shouldn't be expensive, just ten or twenty yuan for one

3. The cost of the operation is really not low. I suggest that if you don't feel at ease, you should try freezing or laser first, and then make a decision. After all, it's better to be careful in your face. There is also a strong suggestion that it is safer to go to a regular hospital.

4. Mole is called "pigmented nevus" in medicine. It is a benign tumor of the skin. It is differentiated from nerve cells. People of different ages and genders may grow mole. Generally speaking, there is no harm to people, but the special parts such as palms, soles of feet and lips need attention. Because these parts are prone to friction, leading to the occurrence of malignant transformation, resulting in malignant melanoma. Therefore, it is suggested that for the special parts of the socket, it is best to remove it in time. The operation can be completed in the outpatient department. After the operation, it's better to make pathological sections of the cut part to observe whether there are changes, whether the cut is clean, whether it is benign or malignant

considering the possibility of malignant transformation e to friction, you'd better go to the dermatology department to decide whether surgery is needed

except for those in special parts, those in other parts of the body are generally divided into intradermal nevus, borderline nevus and mixed nevus. Intradermal nevus is more common, generally protruding on the surface of the skin, larger, more round, black, there may be hair on it, this kind of nevus is safe nevus, generally does not need treatment. Junctional nevus usually appears at the junction of epidermis and dermis. It does not touch higher than the skin surface. It is generally hairless and relatively black. If there is damage, pain, running water, or satellite foci around this kind of pit, it indicates malignant change and should be removed in time

in addition, we need to remind that we should not blindly use laser, drug spot mole and other methods to remove the deposit. Because if the laser is not done well, the surface of the memory is clean, in fact, it can not be completely eliminated; Repeated use of laser treatment can make the memory worse. The method of drug Spot nevus removal is not complete, repeated stimulation also has the possibility of malignant transformation.

5. To go to the dermatology laser clinic to ask if it can be done, if the laser can not be done, the doctor will ask you to go to surgery for surgical treatment. But now many top three hospitals are not willing to do outpatient surgery, so be sure to go to the surgery again to say hello to the doctor and then register.

6. The name of this TV play is never let you go.
I've seen it two or three times, and my favorite one is military adviser Lao Lu. It's really Mr. Du yuan. You're right<

director: Lei Xianhe
screenwriter: Guo Zhongshu
Starring: Ren Chengwei (as Wei Tao)
Pan Yuchen (as Wu Meng)
Zhao hengxuan (as Chen Yilong)
Du yuan (as Lao Lu)
Lin Peng (as Liu Xiangjing)
hope to adopt

7.

When discussing the metallogenic series of hydrothermal sedimentary deposits, this book has in fact discussed in detail the mineral resources or deposit assemblages and their characteristics related to hydrothermal sedimentation in certain geological period and certain tectonic environment in some areas of Guangxi, which has laid a foundation for the division of metallogenic belts. Since the hydrothermal sedimentary events are related to the extensional tectonic environment, especially to the synsedimentary faults and related sedimentary basins, the discussion on the metallogenic belt of hydrothermal sedimentary deposits in Guangxi is mainly based on the corresponding extensional depression area. The related depressions include the Proterozoic Early Paleozoic rift belt in northern and Eastern Guangxi, the early Paleozoic rift belt in southeastern Guangxi, the Devonian strike slip fault belt in central and Northern Guangxi, the late Paleozoic rift belt in northern Guangxi (Danchi), the Devonian Early Triassic rift belt in southwestern Guangxi, and the early Middle Triassic rift belt in Northwestern Guangxi. Accordingly, there are six main metallogenic belts in the area, namely, the Proterozoic Early Paleozoic rift iron tin vanadium tungsten copper barite metallogenic belt in northern Guangxi Eastern Guangxi, the early Paleozoic rift lead zinc copper tungsten polymetallic metallogenic belt in southeastern Guangxi, the Devonian strike slip fault lead zinc barite pyrite metallogenic belt in Central Guangxi northern Guangxi, and the late Paleozoic rift manganese tin polymetallic metallogenic belt in northern Guangxi (Danchi), The Devonian Early Triassic rift manganese lead zinc barite pyrite metallogenic belt in Southwest Guangxi, and the early Middle Triassic rift gold metallogenic belt in Northwest Guangxi

(1) in the Proterozoic Early Paleozoic rifted Fe Sn V W Cu barite metallogenic belt of Northern Guangxi and Eastern Guangxi, many rifting activities occurred in Guangxi ring the Proterozoic. In the early Neoproterozoic, the Danzhou group was deposited in the north of Guangxi. In the early Sinian, the Chang'an, Fulu and NANTUO formations were deposited in the north of Guangxi. In the east of Guangxi, the yingyangguan formation was deposited. In the late Sinian, the argillaceous and siliceous formations were formed in the north of Guangxi. In the east of Guangxi, the Xialong formation slate intercalated with dolomite and dacite. The Cambrian system is divided into Qingxi formation and Bianxi formation, which are mainly composed of terrigenous clastic turbidites with siliceous rocks

The ore deposits in this area are tin deposits (Wudi, Yidong, Jiumao, etc.) formed in Mesoproterozoic in northern Guangxi, iron deposits (yingyangguan, Sanjiang) formed in both sides of the continental basin in Neoproterozoic, and barite deposits (liwang, Banbi) formed in late Sinian Early Cambrian. In the Early Cambrian, Vanadium Deposits (luochenghuai group) and tungsten deposits (Niutang boundary) were formed, while in the middle and late Cambrian, Qinjia copper tin iron deposit was formed

Therefore, the Proterozoic in this area is characterized by iron tin mineralization, but the mineralization is weak. The tin deposit has not formed a real ore body. It is mainly proced as the source bed of tin mineralization in the later stage. The scale of iron deposit can reach medium and large scale. There are tungsten, vanadium, copper, tin and barite deposits in Cambrian, in which scheelite and vanadium mineralization still have good prospecting prospects

Second, the early Paleozoic Pb Zn Cu w polymetallic metallogenic belt in southeastern Guangxi is a part of Dayaoshan marginal sea in Caledonian. The Cambrian Silurian strata in the area are continuously deposited, with multi-stage submarine volcanic activities (Yang Bin et al., 2000a). The sedimentary environment is mainly shallow shelf sub deep marine facies, only the Cenxi area is sub deep sea, deep sea shore shallow marine facies. The deposits in this area include lead-zinc iron ore (Xiashui) and copper silver polymetallic ore (jilongding) in Ordovician, tungsten molybdenum ore (youmapo, Liusu, Daling and Pingtang) in middle and Upper Ordovician and Lower Silurian, and lead-zinc ore (Fozichong and Dongtao) in Lower Silurian. Therefore, this area is characterized by Pb Zn Cu w polymetallic mineralization, in which the scale of Pb Zn is large and can reach large scale. There are some tungsten (molybdenum) ore occurrences, which can be regarded as the source bed of tungsten (molybdenum) mineralization in the later stage, providing new information for the exploration of hydrothermal sedimentary tungsten (molybdenum) deposits in this area. It can be said that most of the polymetallic mineralization occurred in this area in the middle and late Early Paleozoic in Guangxi

(3) lead zinc barite pyrite metallogenic belt in Devonian strike slip fault depression of central and Northern Guangxi, which includes Huanjiang Rong'an area in northern Guangxi on the southern margin of Jiangnan ancient land and Laibin, Wuxuan and Xiangzhou area on the west side of Dayaoshan ancient land, belongs to a part of Devonian sedimentary basin in Hunan and Guangxi, and is the result of intraplate rifting since early Devonian, At the same time, it is controlled by the regional Longsheng Lengshuijiang synsedimentary fault zone (Wang Jian et al., 1998; Li Wenyan et al., 1991). The upper Paleozoic, especially Devonian, is widely distributed in the area. The sedimentary environment is mainly the limited platform, semi limited platform and open platform facies belt of carbonate platform facies area, as well as the reef (Beach) facies belt and platform basin facies belt, and the tidal flat facies belt of shore clastic facies area. The hydrothermal sedimentary deposits in this area are mainly early Devonian lead-zinc barite pyrite (Wuxuan Lemei, Pengcun, Guli, Panlong, jiuya) and middle Late Devonian barite (Laibin Gutan, Xiangzhou Pancun) in Central Guangxi, and middle Late Devonian lead-zinc deposit (siding) and lead-zinc pyrite (Beishan) in northern Guangxi, followed by early Devonian Baoan lead-zinc deposit. In addition, Guiping xijikeng, Fenghuangling, Qingfeng Pb Zn deposits and Mugui Mn deposits in the southwest of Dayaoshan ancient land may also belong to the southern extension of the metallogenic belt. The mineralization in the area is obviously controlled by Longsheng Lengshuijiang synsedimentary fault zone and its derived faults, resulting in the formation of early, middle and late Devonian layered deposits and some early and Middle Devonian vein deposits e to different emplacement mechanisms of deep circulation hot brine. This area is an important lead-zinc barite pyrite metallogenic belt in Guangxi, which still has great prospecting potential

(4) the late Paleozoic rift manganese tin polymetallic metallogenic belt in northern Guangxi (Danchi)

this area is commonly known as the Danchi metallogenic belt. Danchi basin is a secondary basin of Youjiang rift basin. It is a rift trough controlled by Ziyun Danchi synsedimentary fault zone. Its southern end reaches Shanglin, Wuming and Nanning. The sedimentary environment is platform trench facies belt and reef facies belt at the edge of platform trench. The late Paleozoic strata, especially Devonian and Carboniferous, are widely distributed in the area. Ore deposits were formed from early Devonian to Early Carboniferous, but mainly in middle and late Devonian, such as tin polymetallic deposits in Changpo Tongkeng, Longtoushan, Lamo, BEIXIANG and Wuxu, and mercury deposits in Yilan and Wanbaoshan. In addition, there are Damingshan tungsten deposit and Dafeng vanadium deposit in Early Devonian, and yizhoulongtou, Tongde and xinchenglimiao manganese deposits formed in Early Carboniferous. Therefore, this area is characterized by Sn Pb Zn Cu sb Hg polymetallic deposits formed in Late Paleozoic, especially in middle and late Devonian, with large scale, often large and super large. This belt is the most important tin polymetallic metallogenic belt in Guangxi, with great prospecting potential

(5) Devonian Early Triassic rifted manganese barite pyrite lead-zinc metallogenic belt in Southwest Guangxi is an important manganese metallogenic belt in Guangxi. It is a secondary basin of Youjiang rift basin. Structurally, it is a Napo Longzhou rift trough controlled by Guangnan Funing Napo fault zone, and Guangnan Napo fault zone is also a regional synsedimentary fault zone. The sedimentary environment is mainly platform trench facies belt, followed by subtidal semi limited basin, open platform facies belt and shallow sea shelf facies belt. There are late Paleozoic strata and Triassic in the area, especially Devonian. The mineral resources in this area are mainly manganese deposits (Xialei, Hurun and tuhu) formed in the Wushan formation or the Liujiang formation in the late Devonian, followed by the Longhua barite pyrite deposit in the Yilan formation of the Lower Devonian, and the Changtun lead-zinc deposit in the Middle Devonian. In addition, Dongping manganese deposit was formed in the Early Triassic, but the mineralization is poor, which is the source bed of secondary manganese deposit

This area mainly refers to the Youjiang rift belt in Northwest Guangxi, which is also a secondary basin in the generalized Youjiang rift basin. From the middle and late Early Devonian, the area began to rift, until the early and Middle Triassic formed the rift basin. Triassic is widely developed in the area, while Cambrian and Devonian Permian strata are distributed in the local uplift area of large depression area. The micro disseminated gold deposits widely distributed in Youjiang rift zone occur in the lower and Middle Triassic. Gaolong, Jinya, Mingshan, luolou, Langquan and Nabi gold deposits belong to hydrothermal sedimentary type. Even the vein like and lenticular gold deposits, such as Ba and Longchuan, which occur in the local uplift area, may be formed by the deep circulating hot water rising and filling along the faults derived from the synsedimentary faults in the basin. They are closely related in the source of the ore-forming hot water, but their emplacement modes are different (Chen Dajing et al., 2003; Xie shiye et al., 2006). Therefore, the area is characterized by micro disseminated gold deposits formed in the middle and Early Triassic, and there is still a great prospect for gold prospecting, followed by late Paleozoic hydrothermal sedimentary gold deposits, such as Maxiong, LONGHUO and so on

9. No, it's from Fengcheng to Nanchang. It's not a bus. It's only a short distance bus

10.

As of August 2019, 11 stations will be set up in the upstream and 11 stations in the downstream of Nanchang bus 168, starting from Honggutan supporting central station, passing through Nanchang first hospital, Nanchang Aviation University, Nanchang International Sports Center, < EM > Nanchang west station < / EM >, Nanchang Ring Expressway, Shanhou highway and Fengcheng station to fengshuihu Park station

in order to facilitate passenger travel, the platform of No.168 (Nanchang Fengcheng) Nanchang west station is moved to the West hub of North Square of No.50

you can find the bus stop 168 in the West hub of North Square of Nanchang west station