gondwana 中文意思是什麼

gondwana 解釋
風瓦納古陸
  1. The development of an atypical hirnantia - brachiopod fauna and the onset of glaciation in the late ordovician of gondwana / owen e. sutcliffe. . [ et al. ]

    岡瓦納古陸晚奧陶統一個典型的赫南特貝屬-腕足動物群的發育和冰川作用的開始
  2. The iridium layer commonly used to support catastrophism fits into this theory as evidence for the extreme volcanism that would have been produced by the eruption of larasia and gondwana

    至於那個支持災變說的銥異常層，則可能是拉拉西亞和岡納德萬噴發時特別強大的火山作用的產物。
  3. ( 3 ) the position ofcoleonyx as the sister group of the other genera, holodactylus and eublepharis is different from most of previous results ; ( 4 ) our results support the hypothesis that the early eladogenesis of the gekkota was associated with the split of eastern gondwanaland from western gondwanaland. divergences within living genera in the eublepharidae. and the eastern gondwana lineages ( diplodactylidae, pygopodidae and carphodactylidae ) may be older than those in the gekkonidae

    Dpctylidae人（ 3 ） g金虎科三個屬之間的關系為（ oleol7n （ mlo由ctrlus十伽7郵ar d ） ，與此前大部分研究結果不同； k ）支持壁虎類蝴蝎早期分化與東、西岡瓦納古陸的分裂相關的假說，現存瞼虎科和東部岡瓦納分支（刺尾虎科、鱗腳虎科和基趾虎科）的分化時間可能較壁虎科為早。
  4. Thus, it can be clearly recognized that the global continents located at near equator and southern hemisphere, showed the characteristics of range along latitude ; chinese continental blocks still located among the laurentia, siberia and gondwana in paleozoic ; following the fast moving of siberia plate to northwards, the amalgamation in north - south direction at the western parts of laurentia and gondwana, subducted the lapetus and rheic oceans, until to form the uniform pangea in the late stage of paleozoic ; however australia and india plates in eastern gondwana move and disperse gradually to southwards, to extend crust and form the paleo - tethys ocean ; the chinese continental blocks and adjacent blocks still located in paleo - tethys ocean, preserved the status of dispersion, gradually moving to northwards, showed the characteristics of range along north - south orientation, until carboniferous and triassic a series of local collisions happened in tianshan - hing ' anling, kunlun, qinling - dabie, jingshajiang and shaoxing - shiwandashan zones, thus the most part of chinese continental blocks amalgamated to eurasia continent

    由此可以清晰地看出，在古生代早期全球各大陸的主要部分都位於赤道附近及南半球，大致表現為沿緯度、呈東西向排列的特徵，中國及鄰區的小陸塊群在古生代始終都處在勞倫大陸、西伯利亞與岡瓦納大陸之間；隨著西伯利亞大陸的快速北移，在勞倫大陸與岡瓦納大陸的西部地區發生南北向拼合，亞皮特斯洋和里克洋的消亡，到古生代晚期形成統一的泛大陸；而岡瓦納大陸的東部（澳大利亞和印度等）則逐漸向南移動、離散，地殼張開，構成古特提斯洋；中國及鄰區的小陸塊群則一直處在古特提斯洋中，保持離散狀態，總體上緩慢地向北運移，並逐漸轉為近南北向的排列方式，石炭紀到三疊紀才在天山興安嶺、昆侖山、秦嶺大別、金沙江和紹興十萬大山等地段發生一系列局部性的陸陸碰撞，使中國大陸地塊的大部分逐漸併入歐亞大陸。
  5. The supercontinent of gondwana had just formed and was located near the south pole

    超大陸岡瓦那開始在南極附近形成。
  6. Eastern gondwana had begun to separate form western gondwana

    盡管盤古大陸依然完整，不過可以聽到大陸開始分裂的隆隆聲。
  7. This formation is dominated by a set of sandstone - mudstone dark clastic rock series which belongs to marginal marine deposit at the end of the gondwana carboniferous - permian glacier period

    該組主要為一套砂巖泥巖的暗色碎屑巖系，屬岡瓦納石炭二疊紀冰川末期的邊緣海沉積。
  8. The long isolation in the different phytogeographical units ( i. e. the northeastern gondwana unit and south china subunit during the early devonian ) and different environment may result in the evolution and diversify of numerous endemics

    不同古植物地理區的長期隔離（也就是，早泥盆世的東北岡瓦納古植物地理區和華南亞區）和獨特的環境可能是造成眾多地方性分子演化分異的原因。
  9. Its sedimentary type has the characteristics of both the stable deposit of gondwana continent and the low energy deposit under coastal conditions, and mainly consists of a set of tidal - flat sedimentary assemblage whose sedimentary environment is related to short - period and small - scale inshore glacier activities

    其沉積類型既有岡瓦納大陸穩定沉積特點，又有濱岸條件下的低能沉積特徵，主要為一套潮坪沉積組合，其沉積環境與短周期小規模近岸冰川活動有關。
  10. The marginal ocean basin ' s formation and evolution model may be as follows : early triassic, rift was formed by extension and splitting in india ( gondwana ) continental margin during it was drifting southward ; late triassic, the rift had been joined in the neo - tethys ocean in the east and converted into initial ocean basin, and ayila - zhongba micro - continental was formed in north of the rift

    洋盆的演化模式是：早三疊世，隨著印度（岡瓦納）大陸向南漂移，其北部邊緣因引張裂解產生裂谷，于晚三疊世向東開口與新特提斯洋主體連通，洋盆初具洋殼性質，北側形成阿依拉仲巴微陸塊。
  11. 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。
分享友人
分享到 Line

分享到臉書