皺褶屬 的英文怎麼說
中文拼音 [zhòuxízhǔ]
皺褶屬
英文
fimbriaria-
Long shimmering brown shirt - - - - - made from iridescent crinkled fabric designed with wrinkles and pleats, this simple shirt is brought to life with some exquisite details in unexpected places
泛著金屬光澤的金屬絲面料經過各種抓皺、打褶的處理，細節出現在各種始料未及的部位，一件簡單的衣物立刻有了別致的設計感。Chagan sag is a secondary tectonic unit in chagandelesu depression, northeastern yingen - eji ' naqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate, with the character of erogenic belt. in working area and its adjacent area, the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase
查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元，其盆地基底為古生代時期華北板塊、哈薩克斯坦板塊和塔里木板塊交接部位形成的陸緣或島弧褶皺帶，具有古生代造山帶的性質。研究區及鄰區印支期侵入巖形成於造山帶強烈擠壓陸內俯沖的構造環境；燕山早期侵入巖形成於由擠壓轉向拉伸、造山帶的增厚陸殼開始發生伸展垮塌的構造環境；早白堊世火山巖形成於造山期后進一步發生伸展垮塌的區域構造環境。Chagan fault depression is a secondary tectonic unit in chagandelesu subbasin, northeastern yingen - ejinaqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc with the character of erogenic belt at the connection region of north china plate, tarim plate and kazakstan plate
查干德勒蘇凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元。其基底為古生代時期華北板塊、塔里木板塊和哈薩克斯坦板塊交接部位的陸緣或島弧褶皺帶，具有古生代造山帶的性質。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。Seen from the structure, this district belongs to the structure region of tethys - himalayas, " sanjiang " fold system, and the fracture - fold zone of lancangjiang river
從構造上看，本區屬于特提斯喜-馬拉雅構造域，三江褶皺系，瀾滄江斷裂褶皺帶。The western hubei - eastern sichuan area is located at the junction belt between the eastern sichuan folded belt in the sichuan basin and xianexi folded belt, belong to eastern extended part, which is similar to the eastern - sichuan structure in many aspects. for example, they share a structural unit, resulting in the same sedimentary history and the same generation - reservoir - seal assembly as each other
鄂西渝東區處於四川盆地川東褶皺構造帶與湘鄂西褶皺帶的接合部位，屬川東褶皺帶東延組成部分，具有與川東相似的沉積發育史與生儲蓋組合；相同的構造發育史與構造形式；類似的天然氣藏類型與保存條件。When we talk about ears, we usually mean the oddly wrinkled appendages on the sides of our heads
當我們提到耳朵，通常指那個生長在我們頭部兩側的奇怪的褶皺的附屬肢體。When we talk about ears, we usually mean the oddly wrinkled appendages on the side of our heads
當我們提到耳朵時，通常是指那個長在我們頭部兩側的奇特的褶皺的附屬肢體。More and more evidences suggest that the fold basement of yangtze block is an integral part of the grenville - aged orogen. the yanbian group, which resulted from post - grenville orogen, outcrops in the panzhihua area, sichuan province. hence, the studies on the geological features and geotectonic implications of the yanbian group can provide some clues to refine the position of yangtze block in rodinia
揚子陸塊在rodinia中的位置是近幾年來的熱點問題，愈來愈多的證據顯示它的褶皺基底是grenville期造山帶的重要組成部分，鹽邊群是揚子陸塊褶皺基底的組成部分，研究它的地質特徵和大地構造屬性，可以為研究揚子陸塊在rodinia中的位置提供重要的地質線索。Geological, geophysical and geochemical research indicate that ore deposits space distribution present belt in nw direction and strip in ne direction is controlled by the lengthwise structure and transversal structure. in the fold - thrust belt, those ore deposits formed in pre - intracontinental - orogenic stage, such as dingqinnong ag - cu polymetal ore deposit, have the character of one orebody beneath one, so it is optimistic to search new orebodys in deep
地質、地球物理、地球化學研究表明江達構造帶礦床在空間上呈現北西成帶、北東成條規律分佈受縱向構造與橫向構造的雙重控制；在褶皺?沖斷帶，陸內造山期之前形成的礦床（如丁欽弄銀銅多金屬礦床） ，常出現礦體多層疊置、礦下有礦的現象，深部找礦前景樂觀。Gasket grooves and folds for cast - metal cable fittings
鑄造金屬電纜接頭用墊片槽和褶皺分享友人