Jadeite raw stone field mouth characteristics Jadeite raw stone several famous field mouth

Jadeite field area field mouth distribution map

The sale of jadeite raw stone is the jewelry industry's most mysterious kind of transaction, her mystery is in the "stone" on the jadeite gambling, and jadeite gambling there are several judgments based on which the field area field mouth is one of the very important basis. Field is the specific location of mining jade; field area is a number of field due to mining age and similar performance and the formation of the region. Different yokohama jade has *** sex, there are special, especially some of the famous yokohama its characteristics are very distinct, so much so that some of the characteristics only belong to a certain yokohama, only to determine which yokohama it belongs to, in order to observe according to this yokohama jadeite jadeite jadeite specificity, to judge this piece of jadeite raw stone betting sex. Therefore, the jadeite gambling industry has a jargon: do not understand the mouth of the people can not bet on the stone.

The discovery and exploitation of Myanmar jadeite has a history of several hundred years. Its mouth such as a starburst prairie fire, the development of today's name up to nearly a hundred, and a group of stars, the fight, as for the small difficult to name the mouth of the field is starry-eyed. According to the type of jadeite raw stone and mining time order, usually can be divided into the whole field area into six big field area: the old field area, Damakan field area, small field area, after the river field area, Lei Ta field area and new field area

MuNa field mouth

MuNa is the Pachang field area in one of the important and famous old field, due to the mining time is long, the reserve is small, the production is relatively low. The site is famous for producing full-color material with uniform color. The jade contains relatively obvious dots of cotton, imperial green, yang green, boxwood green, and once produced yang green full-color glassy material with occasional seedling green with good water head. The cracks are relatively few, and the variations of the species are large, ranging from bean seeds to glass seeds, with bean seeds, glutinous bean seeds and glutinous seeds predominating, and ranging from medium to coarse jade to fine jade. Jade quality is delicate, with "oil", seed old bottom good, few problems, the general bottom with white or floating emerald green, ice and glass seed green full green is extremely rare, so there is a gamble, especially the "masked material", the risk is also relatively large. Muna field mouth of the layers of mining crust characteristics: the first layer of jadeite raw stone almost all have yellow sand crust, the second layer of red sand crust, with wax skin, the third layer of black sand crust, the fourth layer of gray and black crust, the fifth layer of mine for the white and yellow crust, most of the wax skin. In short, the stone gamblers on the Muna old field mouth of the stone is more love, some people describe the "Muna stone": the sea and sky a color, a little snowflake, the beginning of chaos, "Muna" supreme.

Hui Ka is located in the southeast of the Xiangdong field, where there are many small rivers converge into the Hui Ka River, and then the Hui Ka River to the north in the Xiangdong to the north of the injection into the fog Lu River. The field area is very large, and the various mining sites are concentrated on both sides of the river, including many sites, such as Zhanjia, Mudong, Gunsend, Jade King, Outer Subaqiong, Lower Subaqiong, Gedongyue, Danggepang, Rikuguqiong, and Mupi, etc. The site is located in the southeast of Xiangdong field area. Some of the field (such as ZhanGa) now mining is containing jadeite upland gravel layer, from top to bottom can be divided into three layers: the upper layer of yellow gravel layer, mostly elephant skin, grayish-white, turn sand, seed old, often out of high color material. The middle layer is rust-colored layer, mostly red pepper oil shells, good and bad, there are high-colored, there is also shit bottom, uneven. The lower layer is black and gray layer, mostly black wax shell oolong. Below the black-gray layer is the visible bedrock, a harder blue-green schist. Overall, the black layer is more developed in the Huika field area, which is an upland gravel layer with a large thickness, and the emerald gravels are of varying sizes, with a high probability of producing good seed and color ores.

Hui Ka

Hui Ka raw stone has three distinctive features: (1) thin crust. Hit the light that can be seen in the water to see the color, the novice temptation is great, but this wax shell material is mostly new field will be card, in Yunnan border market a lot, often cut out *** raw body (i.e., water froth and emerald *** raw). (2) more cracks. Most of the ordinary material in the meat of the fine cracks more, which is also the most critical factor in the betting will card. (3) skin color miscellaneous. Gray-green, gray-black mainly, good and bad transparency, uneven distribution of good and bad water, but green water is often better. In short, will card old field mouth of the stone, due to possible out of the unique high green, by the favor of the gambler and collector, especially with the gambling and characteristics of the wax skin, quite attractive. It can be said that a little green is hard to find, there is green into a piece, "Huika" supreme.

Back River

Back River field mouth back river field area is located in the cut bottom county east of about 40 kilometers, large and small distribution of more than a dozen field mouth, due to these field mouth basically distributed in the cut bottom of the river tributary, so that place out of the material we are accustomed to call the back of the river stone. After the river field area in 1963 began mining, now most of the field is basically not out of material. Houjiang field mouth is the only place not out of the brick material, most of the color material, good species, bottom good, good water, small pieces of more, generally a few two to a few kilograms, not out of the big material, not out of the glass ground, most of them like the size of an egg, the general color is relatively light, but there are also colored old species of the old. Houjiang stone generally out of the bracelet, but can be out of the ring. Houjiang stone also has a characteristic, that is, the color is not afraid of light, as long as the species is old enough, polished after the color will become darker, the industry called this phenomenon for the flip color, the color will be more and more green with the prolongation of time.

There are two main types of Houjiang stone: the first type is the flood alluvial layer by the side of the mountain, this flood alluvial layer is covered by a layer of slope deposits, locals call slope deposits for the "gross layer", the gross layer (slope deposits) from the top of the mountain about 1 meter thick, the more to the foot of the mountain, the thicker it is, up to 8-10 meters, with the gravel layer in the slope deposits. The gravel layer is below the slope deposit. The second type is the modern riverbed and rambling type, which is divided into the old Houjiang Jade and the new Houjiang Jade. The new Houjiang jade is produced in the lower part of the alluvium, while the old Houjiang jade is produced in the bottom of the alluvium.

The characteristics of the old Houjiang: the jade skin is gray-green, the individuals are very small, rarely exceeding 0.3kg, mainly water stones, grinding roundness, shape and size are similar to mangoes. Sand skin color a variety of, jade is fine, often with wax shell. Generally, the jadeite produced is often full of green and high emerald, with good translucency and tight structure. The so-called "ten Houjiang nine water" made out of the finished product to take goods is very high, after polishing the color will increase, the so-called "put the hall".

The characteristics of the new Houjiang: skin thicker than the old Houjiang, the same wax shell, individual than the old Houjiang, generally within 3kg, water and bottom than the old Houjiang much worse than the old Houjiang, the finished product polished color will darken, generally speaking, even if it is full of Cui's new production of Houjiang out of the finished product is very difficult to become a high-grade emerald.

Moxisha

Moxisha is located 2 kilometers southwest of Longken Zhai next to the Pachang highway, here for the upland gravel sedimentary sand mine, producing fine texture of the glass seed, icy jadeite raw stone. The deposition of jadeite-bearing gravel is characterized by a yellow sandy gravel layer on top and a gray-green gravel layer below. According to the "jadeite original stone journey" description: Moses sand field mouth gravel soil and sand mixed, jadeite ore layer is relatively loose, from the surface to the deep layer in turn for the yellow and red sand skin, yellow and white sand skin (gravel skin layer is thicker), cobblestone feet, yellow and blue stone feet (gravel skin layer is thinner), small cobblestone feet, blue and yellow mixed stone feet, hair, blue stone feet layer, the production of jadeite individual smaller, jade quality is high, often up to the bottom of the glutinous bottom to the bottom of the glass. The small hill arching up opposite to the mouth of the Mossy Sand field is the Mossy Sand-Glass Tribute, specializing in glass-bottomed jade, usually around 4-5 kilograms, with no large pieces of material. Since 1971, when Hong Kong and Taiwan jade merchants processed the colorless jadeite discarded by the Burmese into the ultimate in jewelry, this high-grade, colorless Mossy Sand stone has become a sought-after and popular item. Although the traditional jadeite industry rejected this colorless jadeite, it embodies the highest texture of jadeite (seed water), but still completely overturned people's traditional concept of aesthetics. The marvelous thing about Moshi Sand is that it produces two of the highest levels of jadeite: glued jadeite and fluorescent jadeite. H. Pan has eloquently discussed the production status of the Mossi sand raw stones:

The crust of the Mossi sand stones is unique, with three main types: white sand skin, gray sand skin, and the less common red sand skin. White sandy skin is the most common, mainly because almost all Mossy Sandstone Heads are low in iron content, and even in red sandy skin, the skin is red while the flesh color is still off-white. As far as its crust is concerned, it can be summarized into three typical features: (1) Desanded crust. This is a typical feature of Mossy Sand stones, some stones are almost completely desanded, some stones are partially desanded, even those stones with sandy skins can always be found in some parts of the desanded feeling; (2) Knife-cutting pattern or honeycomb epidermis. Clear knife-cut surface lines are visible in some of the stones with Moses sand, and round or irregularly shaped pits with dripping surfaces are visible in most of the stones, sometimes very much resembling honeycomb surfaces; (3) Uneven, mounded epidermis. This is very common in those Mossy Sand stones with multiple phases of waterway filling, and sometimes these are closely related to the bluish color, and the raised areas often show a darker crust, caused by the differential hardness of the seed water changes.

If the Mossy Sand stone is grayish-white in color, the flesh is nearly rice soup, and cotton is large. Rubbing mouth if the dark gray, meat is close to ice species. Rubbing mouth is black, its meat for the glass species, to make the finished product after the light is very live. This after light is very live according to today's saying called "firefly", white cotton point is not obvious (commonly known as "cotton off"), as long as there is a hint of green in the meat, then in the finished product will be refracted into the full color (commonly known as "put the hall"). (commonly known as "put tang"). The reason why the gray is the reason for the glutinization, because the species is not enough, coupled with more cotton, so the crust wrapped under the rub mouth in the light reflection, can only present its own color, coupled with the color of the crust gray, the same can be proved that the dark grey and black black is also the same, especially black, because of the species is good, the water is sufficient, translucent, so the rub mouth in the light into the meat when the color of the crust is also reflected out.

Damakan

Damakan is located in the southwest of Xiangdong field area, located in the lower reaches of the Wulu River, including Gedi mill, Songdui, Wamakan, Baxidong, Gongma mill. The field area of the river valley is wide, flat terrain, the formation of alluvial small plains, all secondary mines, emerald gravel layer thickness is small, generally about 5-7 meters. The base is dark gray schist, due to weathering and become black mud layer, locally known as "mud layer", above the base for the yellow layer, the top for the sand mud layer. Damakan jadeite gravel is mostly white and yellow sand skin, no black sand skin, which is one of the important differences between Damakan and other fields.

(1) Damakan jadeite gravel rolling round generally better, jadeite gravel individual smaller, more than 5kg few, this is related to the geographical location of the site, Damakan in the fog Lu River downstream, due to the location of the plains, the water flow rate slows down, the gravel carried by the natural smaller.

(2) Damakan raw stone is very popular with stone enthusiasts, because out of the so-called "yellow with green", many beginners with a flashlight to see, super beautiful, mistakenly thought that this is ice, glass species, in fact, the yellow color under the light is jadeite crust under the fog, and is not really the meaning of the yellow Fei.

(3) most of the green of Damascus pick up the color blue, for this point to pay special attention to, Damascus there is a wax shell of emerald no fog, cut generally skin and flesh are not divided.

(4) Damakan produced small water stone, after a long time and long distance handling, moisturizing, smooth skin, often produce top glass seed, so in the glass seed jade, the best quality when the Damakan rather than Moxisha.

(5) Damakan field area between the different yards between the jadeite crust performance varies greatly, which Damakan yards mouth of the jadeite crust is thicker, gray, and the skin and flesh mixed, the crust must be under the fog, fog, fog color more red, yellow, black, white, red, black fog, the bottom of the fog gray, yellow, white fog, the texture is good.

(6) general "ten fog nine water", where the crust and yellow mingled difficult to distinguish, its jade color blue, and more than showing the state of the honeycomb, the color brown, reddish-yellow, grey, rare wax shell.

(7) Damakan stone almost all have fog layer, its main feature for the color string skin, fog string skin, fog wrapped in color, fog eat color, skin and flesh difficult to distinguish.

(8) Damakan half mountain half water stone yellow shell yellow fog and thin skin, can be gambled. If the thick skin and fog black, the bottom gray water short, green is often blue, and no rebound, can not bet.

Field mouth characteristics: the third layer of the mine, most often see yellow Fei skin, orange Fei skin, red and yellow Fei skin, there are also weathered skin. Under the skin is often "yellow fog" (i.e., yellow Fei), yellow Fei in the green is commonly known as "yellow folder green", the outer skin is relatively thin, the block size of small people see, there are also large pieces. Often produces bean green or melon green, there are also green under the skin, occasionally there will be a good head of full green Gao Cui, lumps of Gao Cui poplar green and seedling green. There are relatively few cracks, and the variations of species are large, ranging from bean seeds to glass seeds, with old field bean seeds, glutinous bean seeds and glutinous seeds predominating, and medium-coarse to fine jade texture. The old and good, yellow jadeite skin and red and yellow jadeite skin, flesh to violet and white mostly, all yellow jadeite is rare, ice yellow jadeite sandwich green is extremely rare, so there is a gamble, especially the weathering skin of the "Mengtou material", the risk is relatively large.

Mo Wanji is located in the northeast of the mouth of the Pachang field on both sides of the tributary of the Mo Wan River, the mining are upland gravel layer of emerald sand mine, the upland gravel layer is cut by the river, about 100 meters deep. The upland gravel layer is cut by the river at a depth of about 100 meters, so the cut gravel layer profile can be seen on both sides. The gravel layer is divided into two layers from top to bottom, the upper layer is red layer and yellow layer, and the lower layer is gray to black layer, semi-colloidal, containing green schist and mica schist. Jadeite gravel often have wax shells, gravel for the semi-rounded to sub-angular shape, mostly for the black WuSha material, thick skin, crust black as if black paint, skin under the fog (many market inside the black skin stone no fog, belong to the new field stone), python with a white fog and pine flowers, generally good seed, high green, block of small will be full of green. At present, Mowanji black osage has been mined as well as Pachang black osage.

"Journey to the Jadeite Raw Stone": Mowanji out of the black skin shell jade, the species meat are excellent, the skin on the python performance can be gambled, betting on the odds of rising is very high, wax shells, black, thick and thin skin have, not good wash.

The piece of gambling stone sold for five hundred million dollars: Mo Wan Ji's Wu Sha as long as there is a performance, it is easy to gamble up, the color is easy to go in, the seed water is good. There is a clear difference between the appearance of Mowanji wushu and wushu from other field entrance, that is, there are dots of white spots on the black outer skin.

Field mouth characteristics: the fourth layer of ore, black tungsten sand skin, block size of small more common, there are also large blocks; often produce bean green or melon green, there are also under the skin green, or oil green, occasionally there will be a good head of water full of green Gao Cui or lumps of Gao Cui emperor green; cracks are relatively few, the species of the larger changes, from the bean seed has been to the glass seed are also available, but also variant, so the gambling is large, the risk is also large.

Nanqi field mouth a class. One of the most important field for the small field area, located in the southern part of the Damakan field area, the left side of the Ndol Lake. The crust is mostly yellow sand skin. And most of the half mountain half water stone or water stone, the crust is generally yellowish brown, here pay attention to distinguish from it is the back of the river. Because the two shell similarity is very high. About the Nanqi field mouth of the statement online information is very little.

The Ongballei open mouth, mostly seed water material. This open mouth is characterized by the kind of young cotton more cracked and heavy easy to change the species, can cotton death. If there is cotton, this field mouth of the stone in the skin above the performance can be seen. Wombaree, the species is generally on the tender side, the water is not clear enough, polished general gloss is not enough.

Wombaree is located in the northwest side of the new factory, close to the location of the old field. Wombaree crust stone grain is obvious, more skin lines, less coarse sand crust, sand fine clip mud, sand feeling is not obvious, thin crust, skin and flesh excessive layer is also thin, skin color yellow reddish mostly, but often the proportion of seed and water is not proportional, water is good and seed is poor, cotton is big, cracks more. It is worth mentioning that there is a new field material and its skin color is more similar, but less stone lines. Pay attention to identify. (Muna's turning sand will be very delicate, concentrated, and sand grains sorted more orderly, thick crust sand layer, stone lines are not obvious, skin color is simple, white that is white, yellow that is yellow, if it is desanded, ice taste bright. Moses sand, turning sand is to be coarser, the texture of the sand grains to be larger, turning sand feeling will be more intense.

Momo bright for a long time, a variety of senior players on the Momo bright field mouth of the jadeite raw stone said differently, due to the relatively small amount of stock on the market, it is also therefore covered with a layer of mystery veil, today we will unveil this layer of mystery for the netizens to help you identify the Momo bright field mouth of the jadeite raw stone.

Momo bright field mouth to the black skin is mainly, mostly fog layer skin shell, skin shell is quite delicate and thin, head is generally longer. Momo bright field mouth of the stone bottom is generally better, clean and no impurities, no cracks, no cotton, give a person a very refreshing feeling, so it is the production of finished emerald more ideal raw materials, higher value.