songpan 中文意思是什麼
songpan
解釋
阿壩松潘-
Basin evolution and hydrocarbon potential in songpan - aba area
阿壩地區盆地演化及油氣遠景 -
The research of large igneous rock province - ermei basalt extrusion - mantle plume shows that songpan - ganzi folded belt is a hopeful target for breakthrough of petroleum exploration, and the key issue is how to make well a coupling and optimization among its faults, structures, traps and reservoirs
根據地震測深、重、磁、電等的探查，發現該褶皺帶深部有一低速高導層，而對大火成巖省峨眉玄武巖噴溢地幔柱的認識深化均表明，四川松潘甘孜褶皺帶是可望獲得油氣勘探突破的靶區，重要的是斷裂構造、圈閉、儲集層的耦合與優化。 -
Geochemical characteristics and significance of triassic sandstones of songpan - ganze block
甘孜地塊三疊系砂巖的地球化學特徵及其意義 -
Songpan - ganzi folded belt in sichuan province of china is a major issue to geoscientists
摘要四川松潘甘孜褶皺帶一直是地球科學家關注的一個焦點。 -
Especially the effects in detail done by non - technicians for ms7. 2 songpan - pingwu earthquake prediction are presented
在此基礎上，就這一時間四川群測群防、專線結合地震工作實踐作了評析和認識。 -
In the link party of qinling - qiliang - kunlun belt, the polyarc - basin systemic characteristic is discussed with strengthen and standout study on the detail relationship analysis between the arc - basin. the bayan har basin thought to be the preexistence of the songpan - garze belt, is a back - arc basin among a series of polyarc - basin systems behind the qiangtang - taniantawong front the arc beginning in the late paleozoic. the eastern margin started as the western passive continental margin of the yangtze block ( d - t2 ), then changed into a foreland basin related to the north china block and the qiangtang block during the middle to late triassic
在秦祁昆侖結合部研究中，加強和突出了精細的島弧盆分析和造山作用關系的研究，探討了秦、祁、昆結合部多島弧盆特徵；通過巴顏喀拉地區沉積特徵，沉積體的空間展布和形態，面式物源供給方式，礦物成分和地球化學背景分析，其沉積盆地屬性總體上反映出一個從過渡地殼-洋殼基礎上發育起來的周緣前陸盆地的發展和演化過程。 -
3 ) according to the dayi conglomerate " s gravel composition and direction when water flowed during geological age, comeback the paleogeograph of the longmenshan foreland basin, speculates that the dayi conglomerate " material source is located in the songpan - ganzi fold belt to the east, the pengguan fault to the west of the western sichuan plateau region
3 ）根據大邑礫巖礫石成分及古流向分析，推測大邑礫巖物源區為松潘-甘孜褶皺帶以東、彭灌斷裂以西的龍門山地區，並恢復大邑礫巖沉積時期巖相古地理，認為大邑礫巖物源主要來自龍門山沖斷帶一側。 -
Is apart from the jiuzhaigou more than 100 kilometers, is apart from the songpan county seat 55 kilometers, south the elevation 3, 658 meters wangxiangtai, north stop to the elevation 3, 150 meter peiriver river valley, the span 3. 5 kilometers
距九寨溝約100多公里，距松潘縣城約55公里，南起海拔3658米的望鄉臺，北止於海拔3150米的涪江河谷，全長3 . 5公里。
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