hercynian movement 中文意思是什麼
hercynian movement
解釋
海嗡動-
This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement, whose tectonic deformation and magma intrusion is fiercely, and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian, it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area, such as a - granite ' s stock, batholiths and diabase ' s dike. there are many fault depressions possible
按照不同構造層，研究了各構造層的構造特徵：基底構造層：受早海西期構造作用的影響，與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的區域擠壓構造作用有關，為一構造變形和巖漿侵入活動強烈的古生代褶皺基底。二疊系構造層：受中海西區域性伸展斷陷作用的影響，盆地及其周緣地區發育與伸展構造有關的構造-巖漿組合，如呈巖株、巖基狀侵位的a型花崗巖以及呈巖墻狀侵位的輝綠巖等。 -
3 ) on the basis of the geochemistry methods of cathodoluminescencean, strontium isotope, carbon and oxygen isotope, trace element, inclusion, etc, pleokarst mechanism have been deeply studied. pleokarst had been brought about in the meteoric water of earths surface, and mainly in the early hercynian movement
3 ）通過陰極發光、鍶同位素、碳氧同位素、微量元素和包裹體等地球化學手段，深入地探討了巖溶作用機制，認為發生於地表或近地表大氣淡水環境，海西早期是區內巖溶作用發生的主要時期。 -
The thermal events of late hercynian movement and late yanshanian movement has great effects on the maturation of source rocks
晚海西運動、晚燕山運動對盆地烴源巖的成熟具有重要的影響。 -
Bachu arch is a large back - thrust uplift. tectonic evolution of its large boundary fault fracture have relation with oil / gas distribution involuntarily. its large boundary fault fracture is basement rift formed in late hercynian period and strongly actived in late himalayan period. oil / gas distribution of bachu - markit have relation with fault interspace distribution. so, this paper also discussed interspace distribution and movement stage of fault
巴楚隆起是一個大型背沖斷隆，其邊界大斷裂的形成演化自然關繫到本區的油氣分佈，隆起的邊界大斷裂多是海西晚期形成的基底斷裂，后在喜山期強烈活動，兼具壓扭走滑性質。 -
However, the true reason that markit slope are so steep is due to intense tectonic movement of late himalayan. as concerned as this hydrocarbon source regional evolution, the key tectonic movements for hydrocarbon accumulation can be divided into three stage : ( 1 ) middle - late caledonian movement ; ( 2 ) late - terminal hercynian movement ( 3 ) late himalayan movement
給合本區的烴源巖演化史，對本區油氣運聚成藏關鍵性的構造運動有三期：中晚奧陶的伽里東中晚期運動；早晚二疊的海西晚、末期運動喜馬拉雅晚期。 -
4 ) through making maps of cave section correlation in the pleokast topography of the early hercynian movement, three karstic circle are recognized in tahe oilfield, and each circle were produced one cave layer, the top cave are earlier than the down caves
4 ）通過海西早期古地貌條件下的四條洞穴對比的大剖面的製作，認為區內普遍發育三個巖溶旋迴，並相應產生三套洞穴層，上部洞穴先形成。 -
3. it is discussed that the buried hill reservoir in this zone experienced karstification in caledonian - early hercynian, indosinian and mid yenshan movement period, and it is indicated that karst formed in late indosinian and mid yenshan movement period are the key periods to form fine reservoir
3探討了該區潛山儲層形成經歷加里東、海西早期、印支和燕山中期運動抬升型巖溶作用，指出印支、燕山中期運動抬升型巖溶是形成良好儲集層的關鍵。
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