西岡山 的英文怎麼說
中文拼音 [xīgāngshān]
西岡山
英文
gunung mat cincang-
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。Carlisle street runs westwards, across a great black bridge, down a hill and up again, by little shops and meat markets, past single - storide homes, until suddenly it stops against a wide green lawn
卡列斯爾大街向西伸展,越過一座黑色大橋,爬下山岡又爬上山岡,經過許多小鋪和肉市,經過一些平房,然後突然對著一大片綠色草坪終止了。Growing only in the upper reaches of the columbia river in north america. in southeast british columbia, the west side of rocky mts. in montana, bitter root mts, the north side of the salmon river in idho and northeast washington. also growing in the east slope of cascade range in washington and northcentral oregon, north - east oregon and south - east washington
分佈於北美洲哥倫比亞河上流域地帶、大不列顛哥倫比亞東南部、蒙他那州洛基山脈西側、愛達荷州薩爾蒙河北側、華盛頓州東北部、同時亦生產于喀斯開山脈東坡、奧斯岡中北部、東北部及華盛頓州東南部。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。The results of combined internal mineral separates and whole - rock sm - nd isochron age for gabbro dikes from : luobusha, angren and xiubugabu in yarlung zangpo ophilite zone are 177ma, 166ma and 173ma respectively. the 4lar - 39ar step heating spectra of rikangba ophiolite suggest that its formation age is also isoma. it indicates that there was a stronger regionally inagmatism during middle - early jurassic, and the time of i75ma was the main period of the magmatic event of yarlung zangpo ophilite
對鄔郁盆地嘎扎村組火山巖剖面的年代學研究表明,該區后碰撞期火山巖的~ ( 40 ) ar - ~ ( 39 ) ar年齡為12 ? 14ma ,侵入其中的花崗巖脈的~ ( 40 ) ar - ~ ( 39 ) ar年齡為10 . 84ma ,與岡底斯西段前人研究資料對比,認為岡底斯帶后碰撞火山巖時代有自西向東逐漸年輕的趨勢。So far, we have been to niang zi guan, ping yao, tai yuan, wutai mountain, the timber bogoda of county ying, and xuan kong si ( a temple in the sky )
今天,我們來到了我們此次五一山西之行的最後一站,大同。在過去的幾天當中我們依次去了娘子關,平遙,太原,五臺山,應縣的木塔,還有懸空寺。明天我們將在參觀完雲岡石窟后返回北京。The lofty and majestic jinggang mountains, covering 670 square km, tower in the central part of mount luoxiao and stretch over the border of hunan and jiangxi provinces
巍巍井岡山位於江西省南部湘贛兩省交界的羅霄山脈的中部,方圓約500里。Through the analysis of subsidence history in the north of western ordos basin, as a result of the terranes northward accretion and the successive collision of the baykala block in the middle triassic, the qiangtang block in the late triassic, the lhasa block in the middle jurassic, the gangdese block in the cretaceous and the subduction of izanagi plate in yanshanian period, the studied region became a intracontinental foreland basin from late triassic to cretaceous
摘要通過對鄂爾多斯盆地西緣北段沉降史的分析可知,晚三疊世白堊紀,由於中三疊世巴顏喀拉地體、晚三疊世羌塘地體、中晚侏羅世拉薩地塊、白堊紀岡底斯地體連續向北增生、碰撞以及燕山期伊佐奈岐板塊的俯沖,盆地西緣北段的響應顯示為陸內前陸盆地的特徵。West montana, north idaho, south british columbia, washington, oregon and central california and west nevada in sierra nevada mts
分佈於西蒙他那、北愛達荷、南大不列顛哥倫比亞、華盛頓州、奧勒岡州、加利福尼亞州中部及內華達山脈西部。分享友人