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84篇 您的检索式:作者名="Cathles L"
    题名 作者 年代 出处 被引量
1海底天然气渗漏系统水合物成藏动力学及其资源评价方法显示文摘根据海底天然气渗漏系统沉淀水合物的动力学模型,计算了海底渗漏系统中渗漏天然气沉淀为水合物的比例。如果BushHill渗漏系统海底水合物或喷溢天然气的化学组成是渗漏系统气源天然气通过沉淀水合物转变而成,则需要约3. 3% ~21. 7% (平均12. 9% )的渗漏天然气在海底沉淀为水合物。结合渗漏系统的活动时间(1万年)和天然气流量(800t/a),沉淀在墨西哥湾GC185区BushHill渗漏系统中的水合物天然气资源为0. 37×109 ~2. 43×109 m3,平均为1. 45×109 m3,与体积和含量评价方法获得的结果基本一致。陈多福 冯东 Cathles L M 2005大地构造与成矿学2005,29,2:17
2一种识别储层非均质性的双示踪剂方法显示文摘根据非均质多孔介质渗流与示踪剂迁移理论,提出一种识别储层非均质性的双示踪剂方法,通过构建考虑层间绕流的非均质单管模型,对双示踪剂方法进行试验验证。该方法利用两种扩散系数存在明显差别的示踪剂(离子型化学示踪剂溴化钾KBr和颗粒型荧光标记示踪剂荧光碳纳米颗粒Cdot)分别反映非均质多孔介质的总孔隙体积和非均质多孔介质内流动区的孔隙体积,识别储层非均质性和评价注入水的波及状况。结果表明:均质条件下KBr和Cdot的穿透曲线基本重合,而非均质条件下KBr和Cdot的穿透曲线产生分离,且KBr和Cdot在多孔介质中的流体置换率或改变率fv值相差较大;在一定的注入速率条件下,通过分析KBr和Cdot的产出规律及其fv值的变化规律,可识别储层非均质性和评价注入水的波及状况,验证了双示踪剂方法的可行性和有效性。姚传进 雷光伦 薛世峰 赵宇石 STEENHUIS T S CATHLES L M 2016中国石油大学学报(自然科学版)2016,40,1:6
3墨西哥湾GC238区冷泉碳酸盐岩的微结构与石化微生物特征显示文摘采于墨西哥湾GC238海底天然气渗漏区浅表层的冷泉碳酸盐岩呈结核状产出,由方解石微晶和胶结物及少量的黄铁矿构成。胶结物由直径为0.1~0.5m的方解石化的球体、卵形体、棒状体组成,充填于方解石晶体之间。冷泉碳酸盐岩结核下表面发育有由方解石化的球体、卵形体、棒状体组成的薄层,其中的一些球状集合体(约5m)断面显示发育有核和外壳的层圈结构。黄铁矿呈草莓状,也具有相似的层圈结构。这种层状结构与活体古细菌被硫酸盐还原细菌包裹的层圈结构相似。样品中所保存的球体、卵形体、棒状体及其所组成的层圈结构可能是石化的甲烷氧化古细菌和硫酸盐还原细菌。管红香 陈多福 Cathles L M Robe.s H H 2008沉积学报2008,26,1:4
4A capless 350℃ flow zone model to explain megaplumes, salinity various, and high-temperature veins in Ridge Axial hydrothermal system 显示文摘Cathles L M 1993Economic Geology1993,88,:1
5How long can a hydrothermal system be sustained by a single intrusive event'? 显示文摘Cathles L M Erendi A H J Barrie T 1997Economic Geology1997,92,:1
6Fluid Transport by Solitary Waves Along Growing Fauhs-A Field Example from the South Eugene Island Basin, Gulf of Mexico显示文摘Revil A Cathles L M 2002Earth and Planetary Science Letters2002,202,2:1
7Phase frac- tionation at South Eugene island Block 330 显示文摘MEULBROEK P CATHLES L WHELAN J 1998Organic Geochemistry1998,29,13:1
8Gas washing of oil along a regional transect offshore Louisiana显示文摘LOSH S CATHLES L M MEULBROEK P 2002Or- ganic Geochemistry2002,33,6:1
9Phase fraetionation and oil- condensate mass balance in the South Marsh Island Block 208-239 area, offshore Louisiana显示文摘LOSH S CATHLES L M 2010Mar Petrol Geol2010,27,:1
10Gas washing of oil along a regional transect, offshore Louisiana 显示文摘Losh S Cathles L Meulbroek P 2002Organic Geochemistry2002,33,:1
11A kinetic model for the patternand amounts of hydrate precipitated from a gas steam:Application to the Bush Hill vent site, Green CanyonBlock 185,Gulf of Mexico显示文摘Chen D F Cathles L M 2003Journal of GeophysicalResearch2003,108,1:1
12A kinetic model for the pattern and amounts of hydrate precipitated from a gas steam: Application to the Bush Hill Vent Site, Green Canyon Block 185, Gulf of Mexico 显示文摘Chen D F Cathles L M 2003Journal of Geophysics Research2003,108,1:1
13Expulsion of abnormally pressured fluids along faults显示文摘Roberts S J Nunn J A Cathles L 1996Journal of Geophysical Research1996,101,28:1
14Gas washing of oil along a regional transect offshore Louisiana显示文摘Losh S Cathles L Meulbroek P 2002Organic Geochemistry2002,33,:1
15Changes in sub-water table fluid flow at theend of the Proterozoic and its implications for gas pulsarsand MVT lead-zinc deposits 显示文摘CATHLES L M 2007Geofluids2007,7,:1
16Hydrothermal convection and uranium deposits in abnormally radioactive plutons 显示文摘1978 Fehn U Cathles L M Holland H D 1978Econ Geol1978,13,:1
17How long can a hydro- thermal system be sustained by a single intrusive event显示文摘Cathles L M Erendi A H J Barrie T 1997E- conomic Geology1997,92,:1
18Types of gashydrates in marine environments and their thermodynamiccharacteristics 显示文摘CHEN DUOFU SU ZHENQ CATHLES L M 2006Terrestrial Atmospheric and OceanicSciences2006,17,4:1
19Permeability of Shaly Sands显示文摘Revil A Cathles L M 1995Water Resources Research1995,35,3:1
20Types of gas hydrates in marine environments and their thermodynamic characteristics 显示文摘Chen D F Su Z Cathles L M 2006Terrestrial Atmospheric and Oceanic Sciences2006,17,:1
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