cathaysian 中文意思是什麼

cathaysian 解釋
華夏系；華夏式的
  1. Comparison of the pan - cathaysian orogeny with the caledonian and pan - african orogenies

    與加里東和泛非造山作用的對比
  2. In this paper, the basic characteristics of neilingding island ? s flora and their relationships with the neighboring floras were studied. the results show : ( 1 ) the vascular flora of neilingding island consists of 127 families, 367 genera and 551 species, of which 38 species of 25 genera and 20 families belongs to pteridophyta ; ( 2 ) the typical families of seed flora are lauraceae, rubiaceae, apocynaceae, annonaceae, euphorbiaceae, moraceae, aquifoliaceae, rutaceae, araliaceae, myrsinaceae, urticaceae, menispermaceae, araceae, palmae, etc. most of them also are the basic elements of cathaysian flora ; ( 3 ) 342 genera of seed plants in neilingding island can be classified to 13 types according to wu zheng - yi ? s " areal types of chinese genera of seed plant " ; the dominant geographical elements are pantropic genera ( 36. 05 % ), old world tropic ( 12. 54 % ), tropical asia ( 11. 60 % ), the total tropical elements made up to 84. 90 % of the total number of genera, but the typical and specialized tropical elements are scanty. most of them mainly distributes to sub - tropic or even to temperate zone ; ( 4 ) comparing the floristic composition of neilingding island with those of the neighboring regions, they is closely related to the flora of hong kong which is situated to the east of neilingding island. they all are belonged to the south china province of cathaysian kingdom

    通過對廣東內伶仃島的維管植物區系進行全面考察、採集、鑒定和研究，結果表明: （ 1 ）共有野生維管植物127科367屬551種，其中蕨類植物20科25屬38種，種子植物107科342屬513種， 12種為廣東新記錄; （ 2 ）種子植物區系的表徵科主要有:樟科、茜草科、夾竹桃科、番荔枝科、大戟科、桑科、冬青科、蕓香科、葡萄科、五加科、紫金牛科、蕁麻科、防己科、天南星科、棕櫚科等; （ 3 ）屬的地理成分以泛熱帶分佈為主，其次為舊世界熱帶及東亞分佈; （ 3 ）通過與鄰近地區植物區系的比較，發現內伶仃島與香港植物區系相似性最高，與古田、古兜山的相似性次之，而與南崑山的相似性較低，它們均屬于華夏植物區系界的華南省。
  3. Multi - arc - basin system of kunlun orogenic belt and the pan - cathaysian continental accretion

    中國及鄰區中新生代大型大陸擴張盆地及其造山作用續
  4. The study areas are located in the jinshajiang zone, nw yunnan and sw part of the shizong - mile zone ( jianshui ), se yunnan respectively, and tectonically belong to the east part of the paleo - tethys tectonic domain. the jinshajiang zone in nw yunnan was a joint terrain between the yangtze and the gondwana blocks, and the shizong - mile zone delineates a suture line between the yangtze and cathaysian blocks

    研究區分別位於滇西北金沙江帶和滇東南師宗-彌勒帶西南段建水地區，構造上位於古特提斯構造域的東段，其中滇西北金沙江帶是揚子陸塊與岡瓦納陸塊的交匯部位，而師宗-彌勒帶則分隔了揚子陸塊與華夏陸塊。
  5. On the origin of cathaysian civilization from the point of underground archaeological studies

    從地下考古看華夏文明的起源
  6. 2. structural systems exposed in the studied area include latitudinal, ns - trending, nw - trending, cathaysian, neocathaysian, and rotated - and sheared - related structural systems, the enrichment and formation of gold and multi - metal deposit were tightly related with the formation and development of above - mentioned structural systems. especially, the compound and joint of those structural systems, and their relation to the geological process in deep, were mainly ore - controlling factors of gold deposits in this area

    2 、遼寧醫巫閭山地區出露的構造體系有緯向、經向、北西向、華夏、新華夏、旋扭構造體系等，這些構造體系的成生演化與該區金-多金屬礦富集成礦有著密切的關系，尤其是構造體系的復合與聯合、深部地質作用與構造體系的聯系，是控制該區金礦的主要構造因素。
  7. 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。
  8. This important tectonic zone parallel to the isotopic geochemical steep zone, which represented a suture line between the yangtze and cathaysian blocks. the geochemical evidence of the jianshui volcanic rocks from the sw part of shizong - mile zone shows that their lithologic types are tholeiites with the comparative flat ree patterns and enrichment in th, depletion slightly in nb, ta, and flat hfse. thus, they may be formed in a back - arc basin with the characteristics between morb and island - a

    該構造帶西南段的建水火山巖地球化學特徵研究表明，該火山巖為拉斑玄武巖，具有較平坦的稀土分配型式， th較富集， nb 、 ta輕微虧損，高場強元素分佈較平坦，具有介於島弧和morb之間的地球化學特徵，可能形成於弧后盆地環境。
  9. The different subsidence history not only demonstrates that the two areas have different tectonic settings, but also proves that the caledonian basin migrated to northwest when the cathaysian plate was gradually subducted toward yangtze plate from southeast to northwest

    這些差別這一方面說明了兩地區具有不同的構造背景，另一方面也反映了華夏板塊由南東逐漸地向北西揚子板塊靠攏，沉積盆地相應地向西北遷移的動力學過程。
  10. There were convergence, collision and shortening in the xiyu, altay ergun, southern yangtze and cathaysian plates, but dispersion and stable sediments in the sino - korean, northern yangtze, qiangtang, gangdise and himalayan plates

    絕大多數板塊基本上保持孤立和離散的狀態，這是早古生代中國大陸各個地塊構造演化特徵截然不同的主要原因。
  11. When the research content and meaning of the orogenic - sedimentology far more is expanding, and enlarging to the global paelogeography. the evolution history in rifting - assemble of southern china continental landmass is investigated with a relationship between sedimentary basin and orogenic belt, which reflects not only a synchronizing but also asynchronies in contrast, the southern china landmass with the global paelogeography. meanwhile it is promoted that the pan cathaysian is an important part of the global paelogeography

    把造山帶沉積學研究內容和內涵進一步擴展，放到全球的古地理格架中，從造山帶和沉積盆地關繫上研究中國南大陸的獨特裂聚演化史，反映出中國南大陸與全球古地理對比既有同步性也有非同步性；進而提出泛華夏陸塊群是全球古地理的一個重要組成部分。
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