connate
英
美
adj. 原（同）生的；同源的；同族的；先天的；性质一致的
英英释义
adj
- related in nature
- connate qualities
- of similar parts or organs
- a connate tomato flower
双语例句
- In1941, Klinkenberg proposed that the slippage effect would occur when natural gas flow through porous media in absence of connate water.
科林贝尔在1941年提出了气体在不含束缚水多孔介质中渗流时出现的滑脱现象。 - The term connate implies born, produced or originated together.
术语原生意指一起出生，产生或同源。雌雄同体的水生陆生或寄生环节动物。 - These characteristics indicate that the ore-forming fluid resulted from fractional crystallization of magma, with the participation of some connate water at the late stage.
根据这些特征可推断出成矿流体源于花岗岩浆的结晶分异，晚期有少量建造水混入。 - Hydrogen and oxygen isotope composition of water in fluid inclusions indicates that ore-bearing hydrothermal solution origined mainly from atmospheric water or deep connate water.
矿物流体包裹体成分反映了两种不同性质热液的活动，氢、氧同位素组成所指示的成矿热水以大气水或地下热卤水为主。 - It has been proved by experiments that there's stress sensitivity in some low-permeability gas condensate reservoirs, and higher the connate water saturation, stronger the stress sensitivity.
实验已经证实一些低渗深层凝析气藏存在应力敏感性，共生水含量越高，对压力的敏感性越强。 - In a word, the effect of connate water and stress sensitivity on development of low-permeability gas reservoir should be paid enough attention.
共生水的存在以及应力敏感性对低渗气田开发的影响应引起足够的重视。 - A study on lithology characteristics and the changing law of formation water salinity in this area proves that the salinity difference between connate water and formation water of water zone is the basic cause of low resistivity.
通过对这一地区岩性特征和地层水变化规律研究，指出原生水和地层水差异是导致低阻储层的根本原因，提出了相应的计算方法。 - Due to the variation of geologic environment reservoir is often invaded by external water, thus, resulting in the property difference between connate water and formation water.
油藏形成后，由于地质环境变化，储层往往会受到外部水系的侵入，从而造成原生水和水层地层水性质的差异。 - Under the action of magmatic heat source controlled by deep-seated faults, the high sulfur gas liberated from the magma, the connate water in country rocks and ore forming materials combined together to form the hot mineralizing fluid.
在深断裂控制的深源岩浆热力作用下，由岩浆析出的高硫气体与围岩封存水、成矿物质相结合，形成成矿热液。 - The thermal flow body rose and into sea along connate fracture uninterrupted adsorbed and enriched minerogenetic elements during long pulse process, and reduced sulfosalt of sea water into H 2S.
沿同生断裂上升喷溢入海的热流体长期脉动过程中不断吸附、富集成矿元素，并将海水中的硫酸盐还原为H2S。