隙泉 的英文怎麼說
中文拼音 [xìquán]
隙泉
英文
fracture spring-
The first stop will be the black sand beach at the foot of the volcano, then proceed to the hawaii volcano national park and visit the volcano museum, and the park s unique geographic features such as the craters, the lava tube and the steaming vents of the volcanoes
接著前往國家火山公園，此地是活火山，隨處可見熔巖縫隙中所冒出的熱氣。在此特參觀火山博物館，特異的火山地理景勝，如火山口熔巖洞地熱噴泉等大自然奇景。To the hawaii volcano national park and visit the volcano museum, and the park s unique geographic features such as the craters, the lava tube and the steaming vents of the volcanoes
接著前往國家火山公園，此地是活火山，隨處可見熔巖縫隙中所冒出的熱氣。在此特參觀火山博物館，特異的火山地理景勝，如火山口熔巖洞地熱噴泉等大自然奇景。Directed by the advance theories of sequence stratigraphy, reservoir beds sedimentology, seismic stratigraphy and petro - geology, measured by exactitude seismic procession, analysis of seismic facies, analysis of single well lithfacies and sedimentary facies, study of macro and micro character of reservoir and diagenesis, this paper study comprehensively the stratigraphy sequence, the type and distributiong of sedimentary facies, reservoir properties, the diagenesis and the evolution of pores of the 2nd and 3rd parts of pingdiquan formation of permian in wucaiwan - shishugou region in jungan basin. we can optimum seek favourable target area and apply the study results on oil field production in order to solve the difficult questions. we mainly achieve several views as follows : l ) establish the sedimential sequence framework of permian formation in studying area and delimint the jiangjunmiao formation of middle dyas series as lowstand system tract, the lower of the second part to the third part of pingdiquan formation of middle dyas series as transgressive system tract, the upper of the second part to the first part of pingdiquan formation as highstand system tract
以層序地層學、儲層沉積學、地震地層學、石油地質學的先進理論為指導，以地震資料精細目標處理、地震相分析、單井巖相分析、沉積相分析、宏觀和微觀儲層特徵分析及成巖作用研究為手段，對準噶爾盆地東部五彩灣? ?石樹溝地區二疊系平地泉組二、三段的地層層序、沉積相類型及展布、儲層物性特徵、成巖作用及孔隙演化進行綜合研究，優選出有利勘探區帶，並將研究結果應用到生產中，解決生產中的難題，主要取得了以下幾點認識：建立了工區內二疊系沉積層序框架，把中二疊統將軍廟組地層劃為低水位體系域，中二疊統平地泉組二段下部三段地層為水進體系域，二段上部一段地層為高水位體系域。Drinking groundwater source in the city of xingtai lies in baiquan karst water system of runoff and emission which is in front of the taihang mountains
摘要邢臺市區地下飲用水源位於太行山前儲存兩種相當豐富的巖溶水和孔隙水的百泉泉域徑流排泄區。The karst water moves from south to north. after moving to jinan city, the karst water is blocked by igneous bodies, the karst water passes through fissures and karst and gushes out to the surface as springs
來自南部補給區的巖溶地下水徑流至老城區附近，遇到巖漿巖體阻隔，在地形低洼部位通過淺部石灰巖巖溶裂隙湧出地表，形成濟南諸泉。Located on fuchuan mountain, yongquan town, jiujiang county, yongquan cave was shaped by the collapse of geological fault
湧泉洞位於九江縣湧泉鄉伏船山，是天然斷層裂隙產生崩塌而形成的溶洞。This immense chasm has been formed by an underground stream which has tunnelled a course through a flaw in the rocks
這個深邃的洞穴是由一條地下暗泉沖刷巖石中的縫隙並使之慢慢變大而形成的。Applicating all kinds of new theories, this research has undergoed die mesningful exploration of the sequence, sedimentary facies, reservoir properties and the evolution of pores of the pingdiquan formation of permian. and the syudying effects can direct our work in fact well
研究應用了各種新理論，對二疊系平地泉組的層序、沉積相，儲層和孔隙及其演化進行了有意義的探索，而且有效地指導了勘探工作。The upper triassic t3x2 is the tight sandstone reservoir in xiaoquan xinchang area, west sichuan. it has the poor physical property of porosity and permeability. the production mainly depends on the growing of the fractures in reservoir
川西孝泉-新場地區上三疊統須二段氣藏屬于緻密砂巖儲層，該儲層孔隙度、滲透率極低，其產油氣能力主要決定於儲層中裂縫的發育情況。分享友人