indian plate 中文意思是什麼
indian plate
解釋
印度板塊-
The contrast of white and dark blue is just like a drawing in indian ink, and is an attracting point of the plate
紋飾層次分明，花紋細密，各層紋飾之間留白，以虛托實紋樣突出，裝飾性強。 -
Areas beneath the mountain belts are under compression while areas beneath basins and the foredeep of the indian plate are under compression
區內造山帶下方均處于擠壓；盆地和印度板塊前緣處于拉張。 -
The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep. under the background of indian plate subducting under asia - europe plate, bachu forebulge was greatly affected by the development of southwest depression and awati depression. almost all of its structure reversed, and as a result of it, both of its south and north boundary migrated. according to its evolution history and its feature, the authors tentatively use both - side migration model to interpret the evolution of compound forebulge. since triassic, almost all the spheres above lithosphere synchronously became flexure. because transpressional stress field became increasingly strong, bachu forebulge continued uplifting and big faults formed. then, bachu uplift, as a whole, slipped upward along those big faults and showed migrating toward thrust zone in plane. in tectonic tranquility, the lithosphere bounded back and in consequence of it, bachu uplift slipped down and showed migration toward craton, at that moment negative inversion structures developed. while the forebulge migrated toward its south and north foredeep, it was very possible that locally extensional stress appeared in the forebulge
在印度板塊向歐亞板塊俯沖的大背景下，巴楚前緣斷隆受西南坳陷和阿瓦提凹陷的影響，新生代時構造體制發生反轉，邊界向南北遷移。根據其發育過程特徵，作者用復合前緣隆起兩端遷移模式對復合前緣隆起獨特的構造發育史進行了解釋：即三疊紀以來巖石圈各圈層同步撓曲變形。隨著擠壓應力場的增大，巴楚隆起在撓曲基礎上不斷抬升，形成幾條大型斷裂帶。 -
Plate, jewels, indian shawls - everything has been pawned and the rest has been sold or seized
餐具，首飾，披肩全都當掉了，其餘的不是賣掉了就是被查封了。 -
To benzilan ( where visitors can view the geological legacy of the collision of the european - asian plate with the indian sea plate ), then on to the dongzhu temple group, and then proceeding to baimang snow - capped mountain, and the feilai temple in deqin, and on to meili snow - capped mountain, mingyongqia glacier, and xidang hot springs from which one can continue on to the yuben fairy waterfall
由中甸為起點，松贊林寺、納帕海、奔子欄（游覽歐亞板塊與印度洋板塊碰撞地質遺址） 、東竹林寺、白茫雪山、德欽飛來寺、梅里雪山、明永恰冰川、西當溫泉、雨崩神瀑。 -
The three orogenic belts of sanjiang, qinling and xingan - mongolia developed in china from south to north, not only record the perfect history of the paleo - asia plates evolutionary process, and also reflect the effects of pacific plate subducting and indian - asia continent collision on continental margin and intern, especially these orogenic belts have experienced the main processes and metallogeny during the collision to post - collision and
我國從南往北發育的三江造山帶、秦嶺造山帶和興蒙造山帶，記錄了古板塊演化旋迴及其成礦作用的完整歷史，也疊加了中新生代太平洋板塊俯沖和印度板塊碰撞導致的大陸邊緣及陸內效應的信息。 -
In the late early cretaceous, the ncc turned into contraction stage again by the influence of the subduction of pacific plate and indian plate
早白堊世晚期該區受太平洋板塊和印度洋板塊俯沖作用影響，華北板塊再次轉入擠壓作用階段，開始了濱太平洋域的演化。 -
Big tsunamis are caused by great submarine earthquakes that mainly occur along the circum - pacific seismic belt, and along the active seismic belt between the eurasian tectonic plate and the indian - australian tectonic plate
引發嚴重海嘯的海底大地震大多發生在環太平洋地震帶或歐亞板塊及印澳板塊之間的活躍地震帶。 -
Indus - tsangpo suture zone is the joint of indian plate and eurasia plate. the study on its evolution history can provide us dynamic evidence for continent - continent collision between indian plate and eurasia plate. then what is the formation mechanism and deformation history for the indus - tsangpo suture zone
雅魯藏布江結合帶是印度板塊和歐亞板塊碰撞的結合部位，研究其演化歷史能夠為解釋印度-歐亞板塊的陸-陸碰撞提供動力學方面依據，那麼本區雅魯藏布江結合帶的形成機制和變形歷史又是怎樣的呢
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