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。
Based on the above, a surrogate models are built for thermal conductibility performance of sandwich panel with " v - type " folded core in this paper, and they can be optimized by multi - subject. the numerical simulation function and optimization design method in condition of lightest weight are shown in this paper
其次，用isight軟體重新設計了40組不同構型的試驗設計點，並以此為
基礎對v型
褶皺芯材夾層板的熱傳導性能構建了可用的代理模型，給出了數值模擬函數和最輕重量條件下的優化設計方法。
Erlian basin is a rift lacustrine basin developed on the hercynian geosyncline folded base in early cretaceous, is featured by simple sedimentary feature, depositional cycle, small lacustrine transgressive, dry climate, salinization lacustrine water and multi - and - near sources
摘要二連盆地是在海西期地槽
褶皺
基底上發育起來的早白堊世斷陷湖泊群，具有湖盆湖浸規模較小、氣候條件乾燥、湖水咸化、沉積旋迴單一，多物源、近物源和粗碎屑等沉積特徵，以及發育巖性地層油氣藏為主的油氣分佈特點。
The author also suggested that the fuxin block developed on the base of the geosyncline in the huabei craton, and had experienced three period process of orogeny, including hercynian folding orogeny in continental margin, mainly indo - sinian to early yanshanian intracontinental fold - faulting orogeny, and late yanshanian to early himalayaian intracontinental range - basin post orogeny
認為阜新地塊是在克拉通裂陷槽
基礎上發育起來的，經歷了海西期陸緣
褶皺始造山、印支?早燕山陸內
褶斷主造山、晚燕山?早喜馬拉雅陸內盆山後（重）造山等過程。
The studied deposit area is located on a monocline geotectonic unit divided by several groups of faults. therefore, the secondary widen transverse and lognitudinal drapes may have great influence on ore forming and location
礦區
基本構造為一個被幾組斷裂破壞的單斜構造，其上發育的次一級的開闊型橫向和縱向
褶皺對礦床的形成和空間定位起著十分重要的作用。
They are paleozoic ~ early mesozoic - fold deformation and the appearance of reversed fault ; mesozoic - the beginning of graben faulting - block period ; early cenozoic - the phase of broke - the forming of block hill ; late cenozoic - the phase of segging - the forming of buried hill. we mark off five kinds of buried hill belts. they include three different kinds of trap on the basis of the cause of trap formation
本次研究在重新認識濟陽坳陷區域構造背景的
基礎上，將濟陽坳陷古生界潛山的形成過程分為四個階段，即古生代早中生代?穩定沉降?隆升?輕微
褶皺變形及逆斷層發育階段、中生代?初步斷陷階段?塊斷期、新生代早期?斷拗階段?塊斷潛山形成期以及新生代晚期?坳陷階段?潛山定型期。
Yili basin is a independent unit of the yili - zhongtianshan micro plate, which is subject to the zhunger - kazakstan plate. it is a superimposed basin which formed on the basis of the folded pre - permian basement, underwent rifting and breaking in permian, depressing and uplifting and multiple deformation and reformation after permian
伊犁盆地是準噶爾?哈薩克斯坦板塊的一個次級構造單元?伊犁-中天山微板塊內的一個獨立單元，它是在前二疊紀
褶皺
基底的
基礎上，於二疊紀擴張、裂解（谷） ，經二疊紀后的坳陷、隆升多期變形、改造而成的復合型改造盆地。
Further imbrication, folding and metasomatism of the ultrabasic rocks occurred at this time.
超
基性巖的進一步疊瓦作用，
褶曲和交代作用發生於這個時期。
The results showed that lamellae were fit tissue for mycelia isolation, and success percentages of mycelia isolation with media pdas, pdaw, bm, pda are 74. 4 %, 35. 5 %, 15. 6 % and 8. 9 % respectively. the results also showed that stipe, mycorrhizae, and soil with the fungi are not fit for tricholoma matsutake isolation
另外，馬鈴薯葡萄糖麥數濾汁培養
基（ pdaw ） 、 bm培養
基、 pda培養
基也從菌
褶2曾東方博士論文:腐生與共生食用菌菌絲體分離、培養及其dna鑒定研究分離到松茸菌絲體，分離成功率依次是35 . 5 % 、巧
The results show that ( 1 ) loops are in general more variable than stems, and in loops a strong adenine bias are observed : ( 2 ) there does not exist a saturation effect in stems, loops or all positions of the 16s rrna gene fragments : ( 3 ) in the molecular cladogram, bagarius forms a sister group with glyptothorax, and euchiloganis forms a sister group with pareuchiloglanis, and exostoma forms a sister group with glyptosternum : ( 4 ) the phlogenetic positions of pseudecheneis, exostoma and glyptosternum are not recognized ; the glyptosternoid fishes are not monophyly although they are defined by 13 osteological apomorphies ; the incongruence of cladograms between molecular and morphological sets may be caused by less informative sites of the 550 homologous sites ; ( 5 ) e. davidi and e. kishinouyei could be the same species according to the genetic distances ; p. sinensis and p. anteanalis could be too
結果表明： （ 1 ）環區平均變異位點較莖區多，有很強的a偏好性； （ 2 ）沒有替代飽和現象； （ 3 ）分子系統樹上?屬和紋胸?屬構成姐妹群，石爬?屬和?屬構成姐妹群， ?屬和原?屬構成姐妹群； （ 4 ） ?屬、原?屬和
褶?屬的系統發育位置不定， ? ?魚類並未形成一個單系類群；可能的原因是所得到的16srrna
基因片段信息位點太少； （ 5 ）青石爬?和黃石爬?可能是同一物種，中華?和前臀?可能是同一物種。
The tectonism in this area can be divided into three phases, that is the folded basement formation and stable ancient land in pre - mesozoic, ancient land cracking phase in mesozoic, the faulted activity and subsidence phase in cenozoic
本區構造變動劃分為三個大的階段，即：前中生代
褶皺
基底的形成和穩定古陸發育階段、中生代古陸裂解階段、新生代塊斷活動及整體沉降階段。
This paper studys basement fold, capping fold, arc structure and magma activity in xingguo area, preseats the concept. of spinning - decollement structure in the area, and makes inquisiton of its mechaninsm of formation
摘要通過興國地區
基底
褶皺、蓋層
褶皺、弧形構造及巖漿活動的研究，闡述了該區旋滑構造的特徵，並對其形成機制進行了探討。
According to characteristics of the seismic data from the low snr region with complex surface, this paper is started from solving the static correction problem and reasonable eliminating all kinds of disturbance in the seismic data from the low snr region with complex surface. through the whole process of seismic data processing which includes a series of processing methods that are suitable for the low snr region, namely, from the choosing of the floating base - level, the static correction in the field and indoors, the eliminating of all kinds of noise before and after stacking, the velocity analysis with high - resolution, the reasonable techniques of deconvolution before stacking and wavelet processing after stacking, to the method choosing of the high - resolution stacking and the reasonable and accurate offset imaging, a set of the complete and effective flow for processing seismic data from the low snr region with complex surface are finally formed, which can meet the need of explo
本文針對復雜地表低信噪比地區地震資料的特點，以解決復雜地表低信噪比地區地震資料靜校正問題及合理剔除各類干擾為出發點，在整個地震資料處理過程中，從浮動
基準面的選取、野外及室內靜校正、疊前疊后各類噪音的去除、高精度速度分析、合理的疊前反
褶積及疊后子波處理技術、到選用高精度的疊加技術及合理準確的偏移成像方法等一系列適合於復雜地表低信噪比地區的處理方法，最終形成一套較完整且有效的針對復雜地表低信噪比地區地震資料的處理流程。
Based on arcgis, discovery and gocad software platform, we built a 3d geological model of the yanjinggou anticline using 3d seismic data in the area
文中
基於arcgis 、 discovery以及gocad等三維軟體平臺，對川西鹽井溝地區地震資料進行精細的解析，得出鹽井溝背料是一個典型的三剪斷層傳播
褶皺，並建立了它的三維模型。
Because the structural interpretation of the 3d model only is of non - uniqueness and uncertainty due to geometric constraint, the finite strain analysis was also applied in the structural interpretation. 184 oriented samples have been drilled at 18 sampling sites in yanjinggou, western sichuan
在川西鹽井溝地區18個采樣點鉆取了184塊定向巖心樣品，通過磁組構的分析結果發現，鹽井溝地區的磁組構
基本上都是弱應變的初始變形組構，
褶皺前翼應變強度比后翼略強。
Santanghu basin, located in the edge of the southern siberian plate, has the double basements of the pre - cambrian crystalline basement and the palezoic metamorphic basement of volcanic - sedimentary rocks
三塘湖盆地位於西伯利亞板塊南緣，具有前寒武紀結晶
基底和古生代火山巖-碎屑巖
褶皺
基底組成的雙重
基底。
Several important tectonic events took place in the chinese continent during the early paleozoic, such as the amalgamation of xiyu plate, forming a unified crystalline basement with the cathaysian plate, development of widespread intraplate deformations in southern yangtze plate, and the occurrence of altay - ergun collision zone
它們與蘇格蘭阿帕拉契亞的加里東事件完全不同，在中國大陸出現了西域板塊完成拼合，華夏板塊構成統結晶基底，南揚子板塊廣泛發育板內褶皺，此時還形成了阿爾泰額爾古納碰撞帶等重要構造事件，而以中朝和北揚子板塊為代表的其他板塊則主要表現為穩定沉積，地塊運移，並呈離散狀態。
