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千层石的地质到底在哪里才是好的呢

文字:[大][中][小] 2016-08-14 19:10:30  浏览次数:

Qianceng stone also calls the overburden rock, belongs to Marine facies sedimentary crystalline dolostone, stone is hard and dense, appearance has weathered layer is very thin, soft; The stone texture is clear, the concave and convex, flat shape, has a certain rhythm, line is fluent, there are twists and turns, ups and downs; Grey in colour black, grey, grey, brown and white, its slightly brown, colour and lustre is compared with the texture coordinate, appear natural, bright and clean; Many strange shape, change multiterminal, yamagata, Taiwan hole shape and natural landscape, has also pyramid, pillar form and characters, animals, such as image, there are both concrete and abstract, beautiful leaves, quietly elegant solemn verve. The original stone is black, colored limestone, thin strip with alternating layers of white, gray stripe dolomite rock, black and white alternate with, commonly known as \"dao\" black and white. Due to the differences in lithology, has produced different dissolution, cambium clear, stripe bump distinct modelling, often appear hills and hole, hole, ravine geomorphologic landscape. Varieties have black and white, squama lotus stone, stone turtle veins, stone, bamboo, stone, fish roe, etc. A black and white way from upper sinian system wangshan group characteristic of the thin film of micritic - micrite, with yellowish green, light gray, gray toner that are thin interbed of fine limestone stone colors. Performance for parallel bar strip combination of black and white. Made in tongshan guo collection area; Squama rock also known as \"money stone\". Turtle grain stone produced in sinian system in the top of mountain and NiYuan group - nine rock formation in a thin layer of white clouds, more than for mud crack formation level structure, formed a crack between layers of texture and complex texture, etc.; Lotus stone produced in the lower Cambrian in fengshan group, geological technical staff known as \"nest\", for formation strata. Visible in tongshan hanwang, etc; Bamboo stone for calcirudite by weathering and karstification and the formation of the stone. The village of class well in hanwang town of mountains; Fish roe stone for oolitic limestone, because the rock is rich in fish roe shaped named oolitic, formed in the depth of small strong warm shallow water environment, water activity.

千层石也称积层岩,属于海相沉积的结晶白云岩,石质坚硬致密,外表有很薄的风化层,比较软;石上纹理清晰,多呈凹凸、平直状,具有一定的韵律,线条流畅,时有波折、起伏;颜色呈灰黑、灰白、灰、棕相间,其棕色稍显突,色泽与纹理比较协调,显得自然、光洁;造型奇特,变化多端,多有山形、台洞形等自然景观,亦有宝塔形、立柱形及人物、动物等形象,既有具象又有抽象,神韵秀丽静美、淡雅端庄。原石是黑色、灰黑色薄层条带灰岩,与白色、灰白色条带白云岩形成互层的岩石,黑白相间,俗称“黑白道”。由于两者岩性的差异,造就了不同的溶蚀情况,形成层理清晰,条带凹凸分明的造型,常呈现山峦和洞、孔、沟壑的地貌景观。品种有黑白道、龙鳞石、龟纹石、莲花石、竹叶石、鱼籽石等。黑白道为产于震旦系上部望山组特有的薄层灰黑色泥晶-微晶灰岩,与黄绿色、浅灰色、灰白色粉细晶灰岩呈薄层互层状的石种。表现为黑白相间的平行条带状组合。产于铜山郭集一带;龙鳞石也称之为“金钱石”。龟纹石产于震旦系九顶山组及倪园组中-薄层白云岩层中,多为泥裂而形成的层面构造,形成了龟裂纹理及复杂的层间纹理等;莲花石产于上寒武统凤山组上段,地质技术人员通称为“大窝卷”,为地层标志层。在铜山汉王等地可见;竹叶石为砾屑灰岩经风化与岩溶作用而形成的块石。产于汉王镇班井村一带的山峦之中;鱼籽石为鲕状灰岩,因岩石中富含呈鱼籽状鲕粒而得名,形成于水深小、水流活动强烈的温暖浅海环境。

千层石是沉积岩的一种,其纹理成层状结构,在层与层之间夹一层浅灰岩石,石纹成横向,外形似久经风雨侵蚀的岩层。因其沉积年代及硅化程度的不同,形成的层理结构迥然有异,沉积年代久远的千层石近于玉质。千层石外形平整,石型扁阔,纹理独特。以此石叠制的假山,纹理古朴、雄浑自然,易表现出陡峭、险峻、飞扬的意境。给观赏者以高山流水,归游自然的欣悦。
Qianceng stone is a kind of sedimentary rock, its texture into layered structure, in between layer and layer a layer of light grey rocks, stone into horizontal, one and weathered erosion of rock. Due to different sedimentary s and silicide degree of bedding structure of the form are very different, the sedimentary qianceng stone to the quality of the jade of very long time. Qianceng stone appearance is smooth, flat stone type rich, unique texture. To fold of the rockery stone, texture and natural, of primitive simplicity and vigorous easy to show the steep and rugged, float in the sky of artistic conception. To the viewer to mountain stream, to swim the natural heart.
千层石的产地分布主要有:沙石峪千层石,主要在河北省遵化市石峪村,其千层石形成于距今12-13亿年的晚元古代蓟县纪,当时的砂岩、硅质岩、白云岩和铁、锰等物质沉积后,经过地质构造运动,沧桑变迁,而形成如今的千层石。灵璧千层石则有土黄色的、土红色的甚至还有白色千层石。浙江千层石产于浙江省衢州市常山县、江山市等地。该石多呈方形,有深灰、褐、土黄等色;表面横向层状纹理层层叠叠,似流云般飘逸;体量小至几十厘米,大至几米,单块重量可达1吨左右;其质地极为坚硬,以硬物敲击石体突出部位可发出金属般的声音;造型姿态或雄伟厚实、或细腻生动、或婉转玲珑,极具欣赏价值。是园林景观、堆叠假山瀑布之佳材。香港千层石产于香港大埔区东平洲岛海岸。该石是由粉砂岩、泥岩、泥灰岩及燧石层构成,经过亿万年地质作用及海蚀、断裂、风化而形成的独特页岩,俗称千层石。石形多扁平,质重坚硬,表面呈黄褐色,亦多阡陌,断面层纹清晰,石间多贝螺、珊瑚。
Qianceng stone producing area distribution mainly include: sand valley qianceng stone, zunhua stone valley village, hebei province, mainly in the qianceng stone formed from 12 to 1.3 billion years ago the late proterozoic jixian, at the time of sandstone, siliceous rock, dolomite and materials such as iron, manganese deposits, through the geological tectonic movement, vicissitudes of life change, and form the qianceng stone now. Lingbi qianceng stone has a khaki and red soil and even white qianceng stone. Zhejiang qianceng stone produced in zhejiang province Quzhou City changshan county, jiangshan city, etc. The stone square, dark gray, brown, khaki color; Surface horizontal layered texture layer cascade folds, like cloud and elegant; Size is small to tens of centimeters to several meters, single piece of weight can reach 1 ton or so; Its texture is very hard, to hard knock stone body protruding points can be metallic sound; Modelling posture or grand thick, exquisite and vivid, or indirect, highly appreciation value. Is the proper material of rockery waterfall landscape, stack. Hong Kong qianceng stone produced in tai Po district tung ping chau island off the coast. The stone is composed of siltstone, shale, marl and flint layers, after one hundred million years geological process, abrasion and fracture, weathering and form unique shale, commonly known as qianceng stone. Stone shape more flat, qualitative hard, heavy, yellowish-brown surface also more buildings, the section layer lines clear, stone more between the screw and coral.

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