背斜式構造 的英文怎麼說
中文拼音 [bēixiéshìgòuzào]
背斜式構造
英文
antiform- 背 : 背動詞1. (用脊背馱) carry on the back 2. (擔負) bear; shoulder
- 斜 : 形容詞(跟平面或直線既不平行也不垂直的) oblique; slanting; skew; bevel; diagonal; askew; inclined; tilted
- 式 : 名詞1 (樣式) type; style 2 (格式) pattern; form 3 (儀式; 典禮) ceremony; ritual 4 (自然科...
- 構 : Ⅰ動詞1 (構造; 組合) construct; form; compose 2 (結成) fabricate; make up 3 (建造; 架屋) bui...
- 造 : Ⅰ動詞1 (做; 製作) make; build; create; produce 2 (假編) cook up; fabricate; concoct 3 [書面語...
- 構造 : structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constituti...
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Due to the multi - period tectonic movement and evolution of mechanical mechanism, syndeposition structures occur extensively in jiyang sag, the base of the sag subsided alternatively during the fault depression, which resulted in sinking of top bending and complicated block structure accordingly, reconstructed the syndeposition intensively, and produced the special structural landscape in combination with all levels of faults and sedimentary formations within it
摘要濟陽坳陷由於受到多期構造運動的影響,在前第三系古地形高點背景上廣泛發育同沉積背斜構造,然而由於坳陷在斷陷期基底滾動式沉降,造成撓曲頂部的塌陷,形成復雜的塊斷結構,使本區同沉積構造發生強烈改造,往往與各次級斷層或沉積地層相復合,表現出獨特的構造景觀。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:正向穹窿型、負向塌陷型、邊隆核陷型:依據巖漿-熱力作用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(熱穹窿) 、中深層侵入型、深部地幔(地殼)熱柱型;提出了熱力構造作用空間分佈的理想模式,將洋陸系統、盆山作用、淺表與中深部殼幔作用、殼幔混合、垂向熱力作用(拆沉)等納入一個整體統一的熱力作用系統中,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。The tectonic style inside the basin is characterized by occurrence of anticlines from the margins to center of the basin, with two limbs mostly starting from reverse faults, developing a tectonic pattern of two faults sandwiching an uplift
盆地內部的構造樣式以自盆地邊緣至中心以此形成背斜構造為顯著特徵,背斜兩翼多發育逆斷層,構成「兩斷夾一隆」的構造格局。The cable - stayed bridge has become a more hopeful bridge style in the great span bridges because of its great merits, such as its great power for span, good performance of structure, brief construction, easy to maintaining, model legerity, lower cost and restricting noises. nowadays, some new bridge structures such as low pylon cable - stayed bridge and no back - stays & inclined pylon cable - stayed bridge etc. have become the ones for the building owners to appreciate when they construct the middle - span bridges
斜拉橋以其跨越能力大,結構性能好,施工簡便,易於維修,外型輕巧,造價便宜,且能限制噪音等優點,已成為大跨度橋梁的一個發展方向。現今,矮塔斜拉、無背索斜拉等新穎的橋梁結構型式,在中等跨度的橋型中已佔有較大競爭優勢,成為許多業主欣賞的新橋型。7. it is indicated the prospects for exploration are beidagang bueried - hill - drape - lik fold oil accumulation belt, baidong structure belt and chengbei fault step oil accumulation belt, which directs the explorations of neogene in qikou depression
7 、指出了有利的勘探區帶是北大港潛山?披覆背斜油氣聚集帶、白東構造帶和埕北斷階式油氣聚集帶,為歧口凹陷上第三系的勘探明確了實施方向。Syndeposition developed in jiyang sag can be classified, mainly based on gravity and the form of sinking, into syndeposit - anticline and syndeposit - nosing structure during the formation and development period
濟陽坳陷發育的同沉積背斜構造可分為同沉積背斜和同沉積鼻狀構造,它們在形成和發展中,重力起主導作用,滑塌是主要形式。Under the effect of regional tectonics, there develop many raws drape anticline and active fault in the front of mountain, and they have especial motion fashion
由於受區域構造長期作用的影響,在北天山山前地區逐步發育形成了多排褶皺背斜及活動斷裂,且運動方式具有獨特性。The east slope area of the chengdao oilfield is located at the eastern - south part of the chengbei lowuplift. it is a covered structure evoluted from the pre - tertiary chengdao hidden hill, with rich petroleum resources
埕島油田東斜坡區位於埕北低隆起的東南部,是在前第三紀潛山背景上發展起來的披露構造,含有豐富的油氣資源,長期以來,對該區成藏條件與成藏模式認識不清。The three gorge reservoir, locating at the suture between two arc tectonic belts of daba mountain and bamianshan, has strong structural deformation and versatile structural patterns
摘要通過分析大量資料並結合野外地質工作,對三峽庫區的區域構造背景及巴東組的主要構造樣式進行了總結,分析了這些地質要素對三峽庫區變形斜坡形成和發展的影響。分享友人