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1.A Study of Completion Fluid Damage to Gas-Bearing Forma- tions of Carboniferous in East Sichuan
川东石炭系气层完井液损害研究收藏指正
2.Oil saturation is one of the important parameters to evaluate fluid property and oil-bearing occurrence in a reservoir, which is mainly calculated by geochemical pyrolysis value, porosity and so on.
摘要含油饱和度是评价储层流体性质及含油性的重要参数之一，含油饱和度的求取主要是靠地化热解值、孔隙度等参数。收藏指正
3.FLUID INCLUSION AND GEOCHEMICAL STUDY OF THETIN-BEARING SKARNS AT RED-A-VEN,SOUTHWEST ENGLAND
西南英格兰Red—A—Ven含锡矽卡岩的流体包裹体和地球化学研究收藏指正
4.Drilling fluid technology for gypsum salt bed and high pressure gas-bearing formation in gasfield Kela 2
克拉2号气田盐膏层高压气层钻井液技术收藏指正
5.It is believed that the exposure of highly reactive surfaces during the wear process along with the high temperatures at asperity contacts act to "polymerize" the fluid, forming a viscous sludge, which inhibits bearing rotation.
研究表明，高温下的金属表面在磨损过程中会产生粘稠的“聚合物”物质，形成粘稠的油泥，阻碍了轴承旋转。收藏指正
6.The source of gold ore is actually an ore-forming fluid storeroom, in which the sub-systems of ore-bearing solution with various properties occur in different levels in the course of migration, differentiation and convergence.
因此，提出了金的液体矿源是通过运移→分异作用→成矿流体的汇聚过程，并构成了不同性状的含矿流体的子体系分层次赋存的成矿流体库。收藏指正
7.In the Au bearing fluid, Au moves mainly as AuCl - 2,AuCl - 4,AuS - 2 ,AuS - 3 and AuSO 3- 3. The Au bearing fluid replaces strongly with wall rocks when it moves into ore forming environments.
在含金热流体中，Au主要以AuCl－2、AuCl－4、AuS－2、AuS－3、AuSO3－3等形式迁移。 当含金流体进入有利的成矿环境中，与围岩发生强烈的交代作用。收藏指正
8.Isotopic chronological study of mineralization show that the fluid inclusion Rb-Sr isochron age for gold-bearing pyrite-quartz veins and pyrite-limonite-quartz veins from the Dashankou gold mine are 354±8.1Ma (2σ ) and 344±21Ma (2σ ), respectively. The two ages are consistent in test errors, indicating the gold deposit was formed in early Carboniferous and related to regional shearing;
成矿作用同位素地质年代学研究表明,大山口金矿区含金黄铁矿—石英脉和含金黄铁矿—褐铁矿—石英脉的石英流体包裹体Rb—Sr等时线年龄分别为354±8.1Ma(2σ)和344±21Ma(2σ),两者在实验测定误差范围内一致,代表大山口金矿形成的时间发生于早石炭世,成矿作用与区域韧性剪切作用有关;收藏指正
9.The ore-bearing fluid of Dabaoshan deposit was relate to magmatic thermal dynamic process and formed hydrothermal sedimentary polymetallic deposit at seafloor .The ore-bearing fluid of Fankou was relate to circulation hydrothermal fluid in deep formation and formed Pb-Zn-Ag-Hg polymetallic middle-lower temperature sedimentary deposit by sea-floor thermal spring overflowing.
大宝山型流体与岩浆热动力作用有关，形成海底火山热液沉积多金属矿床；凡口型流体与深部建造的循环热液有关，形成中低温海底热泉喷溢沉积铅锌银汞矿床；红岩型流体与盆地成岩压实水有关，形成低温单一黄铁矿矿床。收藏指正
10.Rb Sr isochron age of fluid inclusion in quartz from quartz veins is the same as that of gold bearing mylonite, suggesting tha t the both types of ore bodies were formed simutaneously in Caledonian period, i n range of 406～409 Ma.
矿石的石英流体包裹体Rb?Sr等时线年龄测定结果为406～409Ma，这两种类型矿石的年龄在测定误差范围内基本一致，属于加里东期成矿。收藏指正
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