塊狀巖 的英文怎麼說

中文拼音 [kuāizhuàngyán]
塊狀巖 英文
massive rock
  • 塊 : 名詞（古時佩帶的玉器） penannular jade ring （worn as an ornament in ancient china）
  • 狀 : Ⅰ名詞1 （形狀） form; shape 2 （情況） state; condition; situation; circumstances 3 （陳述事件或...
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 塊狀 : bulk; massive塊狀播 sowing in patches; 塊狀採伐 group cutting; 塊狀結構[構造] [化學] block struct...
  1. The nickel mineralization is contained in a layered basic mass if surrounded and underlain by an archean gneiss complex.

    此處鎳礦化產於一層狀基性巖塊內，其四周和下面都為太古代片麻巖雜巖圍繞。
  2. Reliabilty analysis model of blocky rockmass stability and its application

    塊狀巖體的穩定可靠性分析模型及其應用
  3. ( 4 ) blocky rockmass with the same age, same rock and same tectonic experience, has gradual change in weathered and unloaded degree, weathering and unloading of the intact damsite granite rockmass in accordance with the law

    （ 4 ）對于同一時代、同一巖性、有著同一構造經歷的塊狀巖體，其風化往往表現為漸進性。
  4. Although rose quartz is usually too cloudy to be used as a cut gemstone, a few exceptional pieces are found with enough clarity and color to make fine gems. most gemmy rose quartz is used as cabochons where the clarity is not as important as the color. rose quartz is also a very attractive ornamental stone and is carved into popular spheres, pyramids, obelisks, figurines and ornate statues

    粉晶原礦大多為塊狀，產于各地偉晶巖中，生長在上層的質地比較好，粉晶的質地易脆，因內含有微量的胎元素而形成粉紅色，如果長時間接受陽光爆曬會失去原有的嬌嫩色澤，常見的人工加工方式是染色，透明度由不透到半透至全透明的都有，非常清澈明亮的天然晶體，我們稱之為星光粉晶。
  5. The massive tripoli is a kind of soft siliceous rock which is composed of cryptocrystalline quartz. the rock could be prepared for active ultra - fine quartz by airflow pulverization and surface modification. the ultra - fine siliceous powder is a kind of high - quality filler in plastics and rubber

    塊狀硅土礦是一種由隱晶質石英組成的松軟硅質巖，通過氣流粉碎與表面改性制備出的活性超細石英粉是一種優質的橡塑填料。
  6. The mine zone is sandwiched between an overlying block of flows, pillow lavas and minor pyroclastics, and underlying agglomerates, tuffs, and more massive diabase bodies.

    含礦帶夾在上覆的巖流、枕狀巖流和少量火山碎屑巖塊與下伏的集塊巖、凝灰巖和塊狀輝綠巖體之間。
  7. Typically the rock is massive, but commonly it is flaggy or schistose.

    這類巖石典型地呈塊狀，但常呈薄板狀或片理化。
  8. However geological information is fully recorded in the remote sensing image, which made it possible for the choosing of this area as a dissection point to extract complex structural information of orogenic belt in west china. taking fully advantage of multi - band image richly bearing concealed geological information in combination with remote sensing analysis and structure analysis, to anatomy the supracrustal composition and structure of orogenic belt with the regional linear structures and their partitioned block and schistous geological masses as the macro - frame ( in corresponding to structure units and structure segments ) and with the rock masses, structure - rock assemblages, line - featured and belt - featured structures as well as penetrative and non - penetrative foliation ( primary stratum and trans position layering ) and folds as the texture and structure elements. the methods of how to distinguish granulite > ductile - shear zone, imposed fold, different deformed belts -

    因而，本文選擇這一地區作為我國西部地區從遙感圖像上提取造山帶復雜結構構造信息的解剖區，充分利用遙感圖像多波段反映物質屬性的特點和圖像處理提取隱含信息的優勢，採用遙感解析?構造解析相結合的研究方法，以區域線狀構造及由它劃分的塊狀、片狀地質體為宏觀骨架（對應于構造解析劃分的構造單元、構造均勻區段） ，以地質體中的巖石巖體、構造巖石組合，線狀、帶狀構造，透入性、非透入性面狀（原始層理、新生面理）和褶皺等構造作為用於解析的結構構造要素，進行造山帶表殼組成和結構構造解析研究。
  9. From sedimentology symbol such as rock assembled, sediment gradus, sandstone grading analysis, protogene sedimentary structure, ichnofossile and logging facies etc and palaeoenvironment background, it is confirmed that shen84 - an12block s34 segment is braid river delta system, not fan delta system ( abrupt slope ). then it can be more partition as braid river delta plain sedimentary assembled, delta front sedimentary assembled and prodelta sedimentary assembled on core and log assembled. and delta plain sedimentary assembled can be identified four microfacies : braided distributary channel, crevasse splay, overbank deposits and interdistributary bay

    沉積微相研究是儲層非均質性研究的基礎，研究區有豐富的巖芯資料和測井資料，通過巖石組合、沉積韻律，砂巖粒度分析、沉積構造、古生物遺跡和測井相等沉積學標志，結合古環境背景，確定沈84 ?安12塊s _ 3 ~ 4段為辮狀河三角洲體系，而不是前人所認為的扇三角洲（陡坡型）體系，在巖芯和測井組合上可進一步劃分為辮狀河三角洲平原沉積組合、三角洲前緣沉積組合和前三角洲沉積組合，其中三角洲平原沉積組合又可識別出辮狀分流河道、決口扇、分流河道邊部和分流間灣四種微相類型；三角洲前緣沉積組合識別出水下分流河道、水下分流河道邊部和分流河口壩三種微相。
  10. The ore is partly massive and partly disseminated (veinlets and speckles) and there is a halo of disseminated minerals in the surrounding rock.

    礦石部分呈塊狀，部分呈浸染狀（細脈狀和斑點狀），圍巖中並有礦物的浸染暈存在。
  11. Conclusion the taihua complex in the area is a metamorphic complex undergone low - angle overthrust from the south to the north and uplifting lately by fault blocking, rather than a mcc

    結論小秦嶺地區的太華雜巖解釋為經歷了從南向北的鏟狀逆沖推覆和後期抬升塊斷剝露的變質雜巖更為合理。
  12. The massive sulfide contains fragments of barren and mineralized gabbro, and schist.

    塊狀硫化物中含有礦化的和未礦化的輝長巖及片巖碎塊。
  13. The age of jinchuan body was estimated between 1300ma ~ 1500ma ; period of time. the age of jinchuan body was estimated between 1300ma - 1500ma ; disseminated ore is about ~ 1217ma ; sideronitic ore is about 960ma and massive ore is about 911 ma

    其成巖年齡可能在13億年到15億年之間；浸染狀貧礦石主要形成年齡約1217ma ；海綿隕鐵礦石主要形成年齡約960ma ；而塊狀礦石形成年齡911ma左右。
  14. Rather researchers believe the mass concentrations are plugs of dense rock from the lunar mantle that rose toward the surface of the basins after impact

    研究人員相信，其質量來自於結塊狀的高密度巖石，這些巖石是撞擊後由月球地函浮升到盆地表面的。
  15. Qimanyuter ophiolite melange crops out 1 - 3 km in width and extends ew - nee about 50 km, parallels to the kunlun mountains. qimanyuter ophiolite melange is composed mainly of serpentinite ( metapyrolite ), peridotite, bedded gabbro, grbbro, diabase sheet and pillow - like and massif basalt as well. associated sedimentary rocks with this ophiolite melange include silicalite, dark gray silicalite and thin - bedded limestone

    該混雜巖帶所包含的主要巖性單位包括：蛇紋巖（變輝橄巖） 、橄欖輝石巖、層狀輝長巖、輝長巖、輝綠巖席、枕狀、塊狀、杏仁狀玄武巖，與之共生的沉積巖為紫紅色硅質巖、深灰色硅質巖、薄層灰巖等。
  16. Three - dimensional discontinuous deformation analysis on surfaces of rock blocks with general model of water pressure distribution

    塊狀結構巖體在一般水壓分佈模式下的不連續變形分析
  17. The ore is partly massive and partly disseminated ( veinlets and speckles ) and there is a halo of disseminated minerals in the surrounding rock

    礦石部分呈塊狀，部分呈浸染狀（細脈狀和斑點狀） ，圍巖中並有礦物的浸染暈存在。
  18. All the mafic and felsic volcanic - hosted massive sulfide deposits are therefore defined as the kunlun type volcanic - hosted massive copper sulfide deposit

    這些基性火山巖型和酸性火山巖型礦床被統稱為昆侖式火山巖型塊狀硫化物銅礦床。
  19. The host rock shows black and compact structure, characterized by alkaline - rich w k

    玄武巖為黑色緻密塊狀，以富堿w k
  20. Based on geological environment, bi - model volcanic series, sedimentary formation and geochemical features of volcanic rocks, it is held that the deposits were most probably formed in the carboniferous back arc rifted environment

    根據礦床產出地質環境、雙峰式火山巖系、沈積建造以及火山巖地球化學特徵，推斷昆侖式火山巖型塊狀硫化物銅礦床最可能形成於泥盆紀石炭紀弧后拉張構造環境。
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