geologic profile 中文意思是什麼

geologic profile 解釋
地質剖面圖
  • geologic : adj. 地質學的,地質的。 a geologic survey 地質調查。adv. -ically
  • profile : n 1 剖面,半面,(雕像等的)側面;側面像。2 外形,輪廓;外觀,形象;型;【航空】翼型,翼(剖)面...
  1. Through the research on the technology of static correction in mountainous region and disturbing wave denoising, it is proposed that the method integrating static correction, migrated imaging with denoising is used to improve the quality of seismic profile in complicated structure area to reflect the underground geologic feature of complicated arcs, the primary effect has been obtained through application of this method in no. 7 lenghu and shizigou areas

    通過重點研究山地靜校正、干擾波去噪技術,提出了利用靜校正、偏移成像、去噪技術相結合的方法,以提高復雜構造地區地震剖面的品質,合理反映復雜地區的地下地質特徵,該方法在冷湖七號、獅子溝等地區的應用,取得了初步效果。
  2. By knowing the surface information of the geologic bodies, the planar section map and three - dimensional section map can be generated along arbitrary directions, which reflect the outer profile and inner structure of the geologic bodies

    提供了從任意方向對三維地質體剖切生成平面或立體剖面圖的方法,使地質體的整體輪廓和內部結構得到直觀的反映。
  3. Combined with geologic condition and infrastructure characteristics, balance three great structure profiles which trend sn with balance profile theory, then analyze the structure style, association form and each detachment further, and calculate 30 % shorten after the stratum deformation variant it turns out to be striking detachment in multiple tectonic levels and different structure deformation variant style in different stage, after the discussion of the structure style and relation between infrastructure and suprastructure

    結合地表地質情況和深層構造特徵,利用平衡剖面原理對三條地質構造剖面進行了平衡,通過平衡后的剖面更好地對剖面所反映出的構造樣式、組合形態及各個滑脫面進行分析,並且計算出變形后地層的變形縮短量為30左右。研究區內深淺層構造之間存在著顯著的多層次滑脫,且不同層次上構造變形樣式各不相同。
  4. Based on the principles of palaeobiology, stratigraphic geology, sedimentology, diagenesis and reservoir geology, taken field profile and drilling cores as research object, and combined with achievement of predecessors, the sedimentary facies, diagenesis essential characteristics of reservoir and controlling factors for reservoir of feixianguang formation in northwest sichuan have been comprehensively studied. both classic and mordern methods have been used in this research. the main confents includes : stratigraphic classification and correlation of feixianguan formation in lower triassic, the rock fexture characteristics, type and forming conditions of rock ; determining dirtributary law of the sedimentary facies in vertical and horizontal direction and distribution in plane and the essetial contronling factors through correlation of sedimentary facies transverse profile and regionnal geologic characteristics ; establishing plane stereoscopic modle of sedimentary of oolitics beach by studying diagenesis

    主要內容包括:對川西北地區下三疊統飛仙關組地層進行了劃分與對比,研究了飛仙關組地層的巖石結構組分特徵、類型和形成條件;通過沉積相橫向剖面的對比,並結合區域地質特徵,深入研究了沉積相在縱、橫向上的變化規律,確定了沉積相在平面上的分佈及主要控制因素,分析了沉積相的縱向演化過程和建立了沉積相的平面立體模式;詳細研究了該套地層所經歷的成巖作用類型、特徵及對儲集空間的影響,建立了鮞粒灘相儲層的形成與演化模式;最後,從沉積相、成巖作用的角度,分析了區內飛仙關組地層的生油潛力、儲層的分佈規律和發育區塊。
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