How to get to Chang'an cultural center from qingshuiwa
The route and stops of Dongguan Chang'an bus No.11 are shown in the figure below, please click to adopt it, thank you

As a rift basin, the intensity of fault activity controls the distribution and migration of sedimentary centers. Due to the strong activity of the fault and the strengthening of normal faulting, the subsidence center is formed on the hanging wall of the normal fault. Because most areas around the lower Liaohe basin are in the state of denudation and there are enough sediment sources, the sedimentary center of rapid accumulation is formed. In different periods, e to the heterogeneity of active faults in different fault zones and different sections of the same fault zone, multiple sedimentary centers were formed
In the fourth stage of Shahejie formation, the subsidence center of Damintun Sag is located in the west side of the east boundary fault near rongshengbao. Drilling revealed that the thickness of the fourth member of Shahejie formation is 813.5m, and the seismic data shows that the thickest is up to 1000m. The average thickness of the whole depression is 400-500m. In addition, 215m dark mudstone remains in well Shen 50, which is located in the eastern margin of the sag, and no marginal facies deposits are found, indicating that the sedimentary range of Damintun Sag in Sha 4 period is much larger than that at present. The western sag has a wide sedimentary range, thick in the north and thin in the south, thick in the east near the tai'an-dawa fault and thin in the West. There are three subsidence centers along the tai'an-dawa fault zone: the northern Tai'an sag, the central Chenjia sag and the southern Qingshui sag. The subsidence center of Taian in the North developed earlier and the subsidence amplitude was large. The maximum thickness revealed by drilling was 1434.19m, which was not penetrated. It was predicted that it could reach 1600m. Niuxintuo oil layer is mainly distributed in Niuxintuo area, with the maximum thickness of 600m. The sedimentary thickness of Chenjia sag in the middle is relatively small, which is estimated to be 600-700m. Only the upper member of the fourth member of Shahejie formation can be seen in Qingshui sag, with a thickness of 600m. A group of NE trending faults on the west slope belt of the Western Sag have local control on the thickness and distribution of strata in Gaosheng and Dujiatai periods. At this time, the eastern sag is still in the uplift area, so far, the fourth member of Shahejie formation has not been found in exploration, so it is speculated that it may be distributed locally in Niuju area During the sedimentary period of the third member of Shahejie formation, the north and south ends of the eastern boundary fault in Damintun Sag moved strongly, forming two subsidence centers of rongshengpu in the South and Santaizi in the north. The maximum thickness of Es3 in rongshengbao settlement center can reach 3500m, and the maximum thickness revealed by drilling is 2050m. The thickness of the third member of Shahejie Formation in Santaizi settlement center is 2000m The subsidence center of Niuxintuo in the north, Chenjia in the middle and Qingshui in the South continued to develop e to the continuous activity of Taian Dawa fault in the western sag. On the one hand, the subsidence center of Qingshui sag in the South subsided sharply, and the water inflow intensified, which made it a deep-water fault lake basin with a wide area. The subsidence amplitude of Es3 reached 2800m, depositing extensive and thick deep-water turbidite and mudstone sediments; On the other hand, a new subsidence center was formed in the shallow sea area in the south of Qingshui. In the later stage, the western depression uplifted as a whole, but the western slope uplifted greatly, and the depression area (subsidence center) also retreated eastwardthe eastern sag began to rift in the third stage of Shahejie formation, especially in the middle and later stage of Shahejie formation, accompanied by strong basalt magma eruption. Due to the difference of fault activity, the subsidence of Es3 in the eastern sag is large at the north and south ends and small in the middle. Niuju, Qinglongtai and ciyutuo areas in the north are controlled by the faults of tsxi, tsdong and tongerbao, forming two subsidence centers of tsxi and niuqing. The thickness of the former Es3 reaches 1300m, and that of the latter reaches 3000m. Niushen 2 well reveals that the 1600m Es3 is not penetrated. In the South Oulituozi area, the subsidence center of zhujiafangzi is formed on the west side of sanjiepaoqian, with a thickness of 1200m. In the southern gold belt area, influenced by the relative falling of erjiegou and Yingkou faults, a graben type settlement center of Jiazhangsi was formed, with a thickness of 2000m. The thickness of the third member of Shahejie Formation in erjiegou sag is more than 2600m. On the contrary, the magmatic eruption of the volcanic rocks in the eastern sag is strong in the middle and weak at both ends
In the second and first stage of Shahejie formation, two subsidence centers still exist in Damintun Sag, but mainly in rongshengpu sag. In the northern part of the western sag, the Taian subsidence center moves southward and eastward to the vicinity of well yue-1, with a sedimentary thickness of 800m. The shape of Chenjia sag is not obvious, and the maximum sedimentary thickness is 1000m. In the southern part, e to the enhanced activity of Dawa fault, the subsidence center of Qingshui sag shifts southward, with a sedimentary thickness of 1600m. In the southern part, the shallow sea sag has a sedimentary thickness of 800m. There are four obvious subsidence centers in the eastern sag, namely, Changtan, zhujiafangzi, Jiazhangsi and erjiegou, with the thickness of 1400m, 1200m, 1200m and 1400m respectively. The South and North members are thick and thin in the middle, with four centers arranged in footprints In Dongying period, the subsidence amplitude of the eastern sag is the largest, and the subsidence amplitude of the north and south ends is large, and the middle part is relatively small. The thickness of Niuju area in the north is 2500 m, that of beach area in the south is 3000 m, and that of Jiedong and zhujiafangzi area is 1400 m. There are many settlement centers such as erjiegou, Jiazhangsi, Jiedong, zhujiafangzi and niuqing. The subsidence center of the western sag has been transferred to the south, and the northern Tai'an sag has been transferred to the vicinity of well yue-1; The subsidence center of Chenjia subsag moved to the south near well Shugu 92 with a thickness of 1000m; The subsidence amplitude of Qingshui sag is the largest in Dongying period, and the thickness of deposition is estimated to be 2800m. Damintun Sag has the smallest subsidence, the center of subsidence is rongshengpu, and the maximum thickness is 900mas a whole, the subsidence center of the lower Liaohe basin has a trend of moving from north to south from the fourth Shahejie formation to the Dongying Formation (Fig. 4-1). The distribution of the subsidence center is obviously related to the intensity of fault activity, that is, the subsidence centers are all distributed in the hanging wall (descending wall) of the normal fault and move with the change of the active part of the fault, At the same time, considering the position change of the relative uplift area and the strike trend of the isopach line, in addition to the NE trending faults controlling the distribution and migration of the sedimentary centers, some EW trending faults also controlled the distribution of the subsidence centers, especially in the Dongying period. In fact, the latter is shown in the second and first-order thickness maps of Shahejie formation. Therefore, from the Dongying period (probably from the second and first stages of Shahejie formation), the NE trending faults as the main body and a small part of EW trending faults controlled the spatial distribution of subsidence center and uplift center of the lower Liaohe Basin ring the Dongying period (probably from the second and first stages of Shahejie formation)
Fig. 4-1 distribution and migration of sedimentary centers in lower Liaohe Basin
bus line: no.808 → No.38, the whole journey is about 20.3km
1. Take no.808 from Humen high speed railway station, pass 25 stops, and reach Bailu intersection station
2. Walk about 40m, and reach Cai station
3. Take No.38, pass 7 stops, and reach qingshuiwa station
4. Walk about 390m, and reach erudite ecation and training center
3 minutes facial cleaning method: correct face washing is the most basic method for the treatment of acne. First, prepare a clean and soft dry towel and mild irritant neutral soap; 2, the perfume in warm water (22-23 degrees) in the rubbing bubble, the more foam the better. Hold up the foam with your hands and wash your face for 1 minutes. Don't push too hard. Stop if you feel pain. Then wash with hot water (38-40 ℃) for 20 seconds, and then change the warm water to wash for 20 seconds. Repeat this for three times. Charm bath is better, the face is about a punch away from the nozzle, while spraying the face (with hot water), while gently tapping the face with your finger belly. Adjust the water temperature and spray for another 20 seconds. 4. Wipe the water on your face with a dry towel, and then gently press your face to absorb water. 5. Finally, apply the lotion with astringent effect. If you feel tight after applying, you can apply it several times. This law must be issued sooner or later. It has obvious effect on early, middle and late acne
● face washing with gauze: after one month's application of the 3-minute facial cleansing method, whether the acne is reced or not, it can be transferred to this method, which belongs to the intermediate face washing method
1. Prepare a towel, soap and a piece of gauze
2, first fold the gauze into a small piece, dip the soap bubble, wash the forehead, chin, nose and so on;
3, then wrap the gauze on the two fingers of the index finger and middle finger, dip in the soap foam, gently wash the center and whole face of the cheeks with gauze; Br />4, finally put gauze around the index finger, dip the soap bubble to gently wipe the soft skin under the eyelids, and stop if you feel irritation or pain. If you still feel pain the next day, it's because you scrub too hard. At this time, at least 4 days of "emergency face washing method" should be implemented, and then 3 minutes of cleansing method should be used to wash the face after no pain
5. Intermediate face washing method: wash every two days in the first week, every other day in the second week, and every day in the third week
● advanced face washing method: after one month of intermediate face washing method, if it is effective, it can be transferred to this method
1. Prepare soap, towel and a piece of cotton white gloves (the thin one is good), and cut off the sixth and fourth fingers of the emperor's hemorrhoids to form three finger covers
2, first hand intact gloves dip in the soap bubble to gently wash the entire face. People with delicate skin can wear fingernails on the index finger and middle finger, and wash the whole face with foam. Br />3, then index finger, middle finger and ring finger with fingernails, soaps with soap foam to gently wash the cheeks, forehead and chin;
4, take off fingernails, only index fingers retain fingernails, dipped in foam gently scrub the lower eyelid skin, and finally wash the water, towel dry.
Super face washing: if acne still exists after the application of the first three methods, this method can be used. It is more suitable for people with acne scars
1. Prepare soap, towel and a soft children's toothbrush
2, rub the soap on the palm of your hand and use a toothbrush. Br />3, gently brush the forehead, chin and other coarsely textured areas with a foam toothbrush, then wash the foam on the face with clean water and dry the face with a clean dry towel.
● emergency face washing: this method can be used not only for acne, but also for those with more wrinkles. Generally speaking, acne skin is oily, if excessive use of skim soap, it will make the skin dry, very sad. At this point, we will use this method to deal with it
1, rub the soap with warm water in the palm of your hand, and then carefully place the foam in a warm basin, gently stirring to form a whirlpool. Br />2, when the water in the basin is about to stop spinning, immerse your face and let the naturally flowing foam rinse the face for 20 seconds. Then immerse your face in another basin with clean warm water and soak the foam for another 20 seconds. For three consecutive times, water and foam should be changed every time.
3. When washing with clean water for the third time, add a few drops of moisturizing oil into the warm water of the basin, and then soak for 20 seconds
4. Finally, repeatedly dry or press the water on the face with a towel
* acne imprint and scar are the eternal pain of many patients with acne. Although the acne on the face has been cured after a period of treatment, it is too late to go to the doctor or the acne has grown too severe before. There are a lot of black, black and red marks in different colors on the acne spots on the face. In serious cases, there are even potholes and scars, which are reminiscent of orange peel or craters on the surface of the moon, This is the so-called "pock scar"
acne scar is caused by infection, inflammation or external pressure. It is often e to the lack of timely and appropriate treatment when the acne attacks. The inflammatory reaction of skin cells causes damage to the skin tissue, resulting in the generation of scars. Because of the variety of acne, there are many forms of acne scar. The more serious the inflammatory reaction is, the more severe the skin tissue is damaged; The deeper the inflamed part is, the deeper the skin tissue is damaged, and the more serious the acne scar may be left in the future
therefore, acne and acne scar are two major aspects that need to be taken into account in the treatment of acne. A complete set of acne treatment plan must be a complete medical treatment combined with internal skin surgery, including timely finding a professional skin surgeon when the disease occurs, early prevention of acne scar that may be formed in the future, and effective treatment of acne that is in attack, And for the acne scar has been formed for surgical correction, in order to minimize the damage of acne on the skin
what can be done to remove the existing acne scar? First of all, let's know the types of pockmarks:
pockmarks can be divided into two types: spots (pockmarks) and scars (depressions or bulges). The color spots are divided into red and black
the red spot is caused by the inflammation of cells in the original acne area, which causes vasodilation. But the blood vessels will not shrink immediately after the elimination of acne, forming a flat red temporary erythema. It will be redder when the skin temperature rises or exercises. This kind of erythema is not a scar. It will graally fade within 4 to 6 months
the black spot is the pigmentation after the inflammation of acne, which makes the skin dark where the acne is longer than the red one. In fact, these black colors will graally disappear with time. Anxious people have to apply some anti melanin ointment or accept the skin change of fruit acid and vitamin C introction
this kind of stains and pigmentation will disappear naturally after a long time, so they are generally temporary false scars, not real scars. Of course, the disappearance of erythema and melanin requires a certain amount of time, otherwise the constricted blood vessels do not contract, and the red will not subside; The pigment that should be taken away by the cells is not taken away, and melanin can not disappear
generally speaking, this kind of false scar will disappear automatically about half a year on average. However, e to different physical conditions, some people will be longer than the average value, for example, one year or even two years. People who can't wait can only use the help of external application, such as anti melanin ointment, topical application of a acid, Rhododendron acid, fruit acid or levo vitamin C, or receiving fruit acid skin change, dye laser, pulse light therapy and vitamin C introction, which can accelerate the disappearance of color spots
true scars can be divided into pits and hyperplastic scars. True scars don't disappear automatically. They need to be treated by a dermatologist
pit scar is a common condition. When the inflammation of acne is too strong and there is too much collagen in the dermis, the pit may be left e to the collapse of the real skin. And many patients with acne like to use their hands to squeeze the acne, if the squeeze is not appropriate, it will greatly increase the chance of suppurative infection, it is easy to turn small acne, small acne into big acne, and then leave scars. Once the cavity is formed, it will not disappear automatically. It's going to have to be laser skinned
hypertrophic scar, commonly known as "crab foot swelling", is usually determined by congenital constitution. It is the most difficult to treat and easy to relapse. This kind of scar is just the opposite of concave scar, which is a kind of excessive hypertrophic scar. It has obvious red protrusion in the place where it grows over the acne, and its appearance is red and swollen. What's more, it will grow up slowly because of scratching or external force stimulation. It mostly occurs in some patients with special constitution. Because the fibroblasts in the dermis of these patients are too active, they overreact in the process of wound healing. As a result, the end of the dermis after injury e to inflammation is not concave, but protruding, becoming hypertrophic skin tissue hyperplasia
the problems of acne scars in youth include the epidermis, dermis and subcutaneous tissue below the skin. The consequences include skin damage, tissue defect and scar formation, which not only cause skin appearance defects, but also affect the normal tissue structure of the skin. In order to improve the problem of pock mark and pock scar, it is necessary for doctors to make diagnosis and evaluation for different types of scar to determine the treatment plan<
treatment methods for black acne scar:
A) use levo-c skin care procts or levo-c ultrasound introction: brighten skin color, promote skin collagen proction
b) use fruit acid skin care procts: simultaneously treat acne and improve acne scar, promote exfoliation of old and waste cutin, help skin renewal, improve pigmentation after acne, Lightening black spots
C) high efficiency whitening procts or whitening courses: slow down deep melanin formation, accelerate melanin metabolism
treatment methods for red acne scar:
A) pulsed light: it can contract microvessels, has the effect of lightening scar, but needs multiple treatment. Pulse light can also increase the collagen of dermis, make the depression no longer obvious, improve the pore size, so it is also suitable for the skin with erythema and slight pits
b) the use of fruit acid containing care procts: simultaneous treatment of acne and improve acne scar, promote the old waste cutin shedding, help skin renewal, improve pigmentation after acne
C) purification treatment: Acne Pore clearance, prevention and treatment of acne
treatment methods for concave scar:
A) peel off of skin keratin with high concentration of fruit acid, promote the exfoliation of aging cuticle, accelerate the renewal speed of keratinocytes and a small number of upper epidermis cells, and promote the proliferation of elastic fibers in dermis, It has good curative effect on superficial acne scar and can also improve the pore coarseness, but it can only be eliminated after several courses of treatment, but it has the advantages of safety and small side effects
b) filling method: the implant (such as collagen) was injected to make the concave part bulge, so as to level with the surrounding skin tissue
C) pulsed light: it can stimulate the proliferation of fibroblasts, thicken the dermis and smooth the pits. At the same time, because pulsed light can stimulate the proliferation of collagen, this method has a certain effect on red pockmarks and newly formed shallow pits
d) deep skin regeneration therapy: for deep acne and pores
bus line: no.831 → No.54, about 8.0km
1. Walk about 350m from jianshazhou to BAXIN Road overpass station
2. Take no.831, pass 1 stop, and reach Zhouxi station (or take No.107)
3. Walk about 120m to Zhouxi Shangye Street Station
4. Take No.54, pass 5 stops, and reach xinzhongyin Garden Station
5, walk about 300m, Arrive at Xiping
The so-called fair faced concrete, refers to no longer use other decoration, decoration methods, will be removed after the concrete directly as the building surface. Architects often use the surface texture of concrete - rough, smooth or special surface texture and traces left by construction as the special visual effect of fair faced concrete
the water absorption rate of concrete surface is relatively high. Without any protection, the concrete will be damaged by sunlight, ultraviolet, acid rain, oil gas, oil, etc. in the natural environment, and graally lose its true colors. The concrete will be neutralized and damaged as time goes on, and its surface effect will become increasingly dirty, affecting the outlook. Therefore, the transparent protective spraying on the concrete surface can not only solve the problem of protecting the concrete and make it more rable, but also prevent pollution and keep clean, and will not darken e to water absorption. Therefore, the color of fair faced concrete buildings can remain unchanged in the rain, unlike urban overpasses, which are filthy when it rains, Therefore, it is also called dry spraying< br />
