stratum super 中文意思是什麼
stratum super
解釋
stratum疊加,重層-
Under the upper pressures belt or minute super pressures of the upper triassic series and jurassic system interface formation, the fluid in the upper triassic series moved along stratum interface, fault and crack network thoroughfare, formed " secondary gas pool " in the jurassic system
上三疊統和侏羅系界面形成的超壓帶或微超壓帶，使上三疊統氣藏流體在壓力差的作用下，沿斷層、地層界面和裂縫網路通道運移，在良好的侏羅系圈閉中形成「次生氣藏」 。 -
The gejiu super - large tin - copper - polymetallic deposit is famous for producing tin. but now the sustainable development of the whole gejiu ore district faces the tremendous challenge, that is to say, the ore in the surface of ground and in the shallow stratum will soon be mined completely. the situation of resources in gejiu ore district is very tension
個舊錫銅多金屬超大型礦區以錫礦生產馳名世界，但經過數十年的開采，大部份探明錫多金屬儲量已經開采消失，多數礦山已受地質保有儲量不足困擾，達不到生產設計能力，部分礦山甚至已到「等米下鍋」的資源危機的境地而難于維持正常生產，個舊市新建礦業有限公司就是其中之一。 -
Through analyzing bed ' s response to wave, in the condition that super - stratum is more hard and second - stratum is more soft in region of interest, super static interstitial hydraulic pressure amplitude die away rapidly between stratums, before in sight of boundary between hard and soft stratum, plane effective pressure increase to max. shear stress reach peak value when bed thickness is approximately 2. 7 meters, then it will decrease to the minimum on the place where the flexible soil has a common boundary with the rigidity, so the boundary is the most destroy plane on engineering. on the basis of reconnaissance in situ, in normal situation of sea, the structure slides to the basin along the boundary
通過對底床在波浪下的響應分析，對于研究區底床上層較硬而第二層較軟的情況，超靜孔隙水壓力幅值在層間交界處迅速衰減，在臨近硬、軟地層交界處前，水平有效應力增至最大，剪切應力在底床厚度大約2 . 7米左右達到峰值，然後減小，到硬、軟層土交界位置，達到最小，因此這個界面就是最容易發生破壞的工程軟弱面，現場勘查證明，即使在正常海況下，構築物也會沿坡以此交界面為滑動面，緩慢向「盆」底滑動。 -
Researches show there are many types of strata pressure, super pressure in certain depth below the bottom of the jurassic stratum, and also overpressure in the whole jurassic stratum in central and southern of mosuowan salient
研究表明該地區地層壓力類型豐富，侏羅系底部及以下地層在凹陷內一定深度以下普遍發育高壓，在莫索灣凸起的中南部侏羅系則整體處于超壓狀態。
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