火山程序 的英文怎麼說

中文拼音 [huǒshānchéng]
火山程序 英文
volcanic sequence
  • : fire
  • : 名詞1 (地面形成的高聳的部分) hill; mountain 2 (形狀像山的東西) anything resembling a mountain...
  • : 名詞1 (規章; 法式) rule; regulation 2 (進度; 程序) order; procedure 3 (路途; 一段路) journe...
  • 火山 : [地質學] volcano; burning mountain
  • 程序 : 1 (進行次序) order; procedure; course; sequence; schedule; ground rule; routing process 2 [自動...
  1. Taowan conglomerate was formed with underwater seismism at early cambrian period and consists of shattering sedimentary rock, tsunami rock, seismic turbidite and seismic volcanic rock. the shattering sedimentary rock consists of folded rock, cracked rock and autobreccia. the seismic turbidite is located in the south of luonan ductile shear zone and is called the narrow taowan conglomerate. contrarily the broad taowan conglomerate consists of shattering sedimentary rock, tsunami rock located in the north of the zone. the seismic sequence of shattering sedimentary rock - tsunami rock - seismic turbidite - seismic volcanic rock - normal sedimentary rock was first found in luonan shanxi and is rare among the reported examples about it, so it is a good example and offers power evidences to study how the southern marginal basin of huabei plate transferred to qinling orogenic belt

    震濁積巖分佈於洛河韌性剪切構造帶之南,屬傳統"陶灣礫巖"范圍和涵義,即為狹義陶灣礫巖而廣義陶灣礫巖包括分佈於洛河韌性剪切構造帶之北的震積巖海嘯巖及狹義陶灣礫巖。陜西洛南地區首次發現的震積巖海嘯巖震濁積巖震巖正常背景沉積地震沉積列之完整在所報導古地震作用沉積列當中實屬罕見,為華北地塊南緣造及深入了解古地震作用提供了良好地段和有力證據。
  2. After the volcanic eruption of multi - phrase cycle - deformation, filling of basin, crustal uplifting event being studied, this dissertation tries constructing the different degree rhythm of magma activity corresponding with crust - mantle dynamic system, studying the crust - mantle deep processes. based on the studies on the characteristics of volcanic rhythm, igneous rocks assemblages, temporal and spatial distribution of igneous rocks, tectonic deformation, the author has util ized the methods of petrology, geochemistry, isotopic geology et al. to do research on the above - mentioned geological problems

    通過多次幕式噴發-構造變形-盆地充填-地殼隆升事件列的釐定,從活動節律特徵、成巖構造組合類型、時空分佈及其演化和構造變形的歷史記錄,利用巖石學、地球化學、同位素地質學等方法,反演深部過與淺部響應等來闡明造,建立與不同級別巖漿活動節律對應的殼幔動力學系統,追索殼幔深部過,已成為當今地球動力學研究的前沿課題之一。
  3. To make the yanshanian volcanic tempral and spatial distribution and evolution law clear, study the relationship of the deep crust - mantle processes and the volcanic rocks, the author selects the typical areas, xishan of beijing, duolun of inner mongolia, west liaoning, as the study areas where the volcanic rocks strata are developed. through the emphasised geological profiles of yanshanian volcanic strata being surveyed, much field work being done detailly, the small volcanic eruptive units have been defined originally, the levels of volcanic activity rhythm being constructed gradually, as a result, a integrated and systemic rhythm of yanshanian volcanic acivity has been constructed

    為了揭示該區燕活動的時空分佈與演化特徵,探討與深部殼幔過的關系,選擇了燕巖地層發育比典型的北京西、內蒙多倫、冀北和部分遼西等地區,系統的測制了燕巖重點地層剖面,通過野外大量的詳細觀察,從建立最小的噴發單元開始,逐步地建立活動節律的級別,結合區域地層對比,建立了一個比較完整的燕活動節律及其級
  4. According to distribution regularity of elements in strata, intrusive rocks, ores and orebodies of the zhongqiuyang volcanogene hydrothermal copper deposit, this paper has elucidated characteristics of geochemical primary anomalies, determined indicator elements related to the ore deposit and their sequence of zoning, established indices for evaluating denudation extent of ore deposit, and formulated geochemical anomaly pattern of the ore deposit

    摘要據鐘丘洋熱液型銅礦床的地層、侵入巖、礦石和礦體中元素的分佈規律,闡明了該礦床的地球化學原生異常特徵;確定了與礦床有關的指示元素及其分帶列;建立了礦床剝蝕度的評價指標及該礦床的地球化學異常模式。
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