穹隆作用 的英文怎麼說

中文拼音 [qiónglōngzuòyòng]
穹隆作用 英文
doming
  • : 名詞[書面語]1. (穹隆) vault; dome2. (天空) the sky
  • : 隆Ⅰ形容詞1 (盛大) grand2 (興盛) prosperous; flourishing; thriving 3 (深厚; 程度深) deep; in...
  • : Ⅰ動詞1 (使用) use; employ; apply 2 (多用於否定: 需要) need 3 (敬辭: 吃; 喝) eat; drink Ⅱ名...
  1. By physiognomy feature, it could be divided into three types of thermal structure : positive dome model, negative collapse model and border dome core collapse model. based on the depth degree or magma - thermal influenced, it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model, superficial volcano eruption hydro - thermalism and hypabyssal intrusive model, thermal anticline ( thermal dome ) model, mid - deep intrusive model, deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure. there are many interaction system could be induced into a systematic thermal interaction, include : ocean - continent system, basin - mountain interaction, superficial and mid - deep crust - mantle interaction, crust - mantle commingle interaction, vertical thermal interaction ( delamination ) etc.

    依據地貌形態分為三類:正向窿型、負向塌陷型、邊核陷型:依據巖漿-熱力影響的深淺程度或深度分為五類: (古)地熱異常群集區、表淺層火山噴發-熱液活動與淺成侵入型、熱力背斜(熱窿) 、中深層侵入型、深部地幔(地殼)熱柱型;提出了熱力構造空間分佈的理想模式,將洋陸系統、盆山、淺表與中深部殼幔、殼幔混合、垂向熱力(拆沉)等納入一個整體統一的熱力系統中,為盆地動力學研究打開了一個新窗口;研討了熱力構造研究方法。
  2. The mechanical genesis of the complicated rock mass is because several times of tectonism in pro - period made the structure of rock mass in the right dam foundation damaged seriously and rock mass alteration made its mechanical character more anisotropy. after that the fractures in the right dam foundation slope were stretched at the beginning of the quaternary period because in the period yakouhoushan mountain quaquaversal dome was blowups quickly. at the same time, the valley trenching of lancang river reach to 800 - 1000 meter in altitude at the right bank in nuozadu dam site

    導致右岸巖體復雜化的成因是,右岸巖體在早期遭受了多期構造和巖體蝕變的基礎上,第四紀早期丫口後山的快速起與當時河谷下切至800m 1000m高程這一特殊因素組合引起了右岸巖體沿原有的斷裂(裂隙)張開,使地下水等風化營力能夠到達坡體較深部位,經過長期的風化卸荷,形成了右岸復雜巖體。
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