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[1]林承焰,王文广,董春梅,等.流体-岩石相互作用定量模拟技术新进展[J].地球科学与环境学报,2017,39(04):491-515.
 LIN Cheng-yan,WANG Wen-guang,DONG Chun-mei,et al.New Progress in the Quantitative Simulation Technology of Fluid-rock Interaction[J].Journal of Earth Sciences and Environment,2017,39(04):491-515.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第39卷
期数:
2017年第04期
页码:
491-515
栏目:
基础地质与矿产地质
出版日期:
2017-07-28

文章信息/Info

Title:
New Progress in the Quantitative Simulation Technology of Fluid-rock Interaction
文章编号:
1672-6561(2017)04-0491-25
作者:
林承焰王文广董春梅张宪国任丽华史祥锋
1.中国石油大学(华东) 地球科学与技术学院,山东 青岛 266580; 2.中国石油大学(华东) 山东省油藏地质重点实验室,山东 青岛 266580; 3.中国石油大学(华东) 油气储层重点实验室中国石油大学(华东)研究室,山东 青岛 266580
Author(s):
LIN Cheng-yan WANG Wen-guang DONG Chun-mei ZHANG Xian-guo REN Li-hua SHI Xiang-feng
1. School of Geosciences, China University of Petroleum, Qingdao 266580, Shandong, China; 2. Reservoir Geology Key Laboratory of Shandong Province, China University of Petroleum, Qingdao 266580, Shandong, China; 3. Research Laboratory of China University of Petroleum-key Laboratory of Oil and Gas Reservoir, China University of Petroleum, Qingdao 266580, Shandong, China
关键词:
流体岩石相互作用定量模拟成岩体成因机制成岩相多尺度成岩作用过程
Keywords:
fluid-rock interaction quantitative simulation diagenetic body genetic mechanism diagenetic facies multiscale diagenetic process
分类号:
P584
DOI:
-
文献标志码:
A
摘要:
成岩体是指在埋藏成岩作用过程中形成的、内部具有成因联系的、不同规模尺度的地质体。从多尺度成岩体研究入手,阐明成岩体中控制流体-岩石相互作用的热力学和动力学条件,揭示流体-岩石相互作用机制,提出以成岩相为核心的多尺度成岩体划分方案,进而归纳总结了成岩体系域、成岩体系、成岩相和成岩亚相不同尺度成岩体的流体-岩石相互作用研究新进展。从单相/多相流体和单矿物/多矿物相互作用角度,将流体-岩石定量模拟划分为长石-流体相互作用定量模拟、石英-流体相互作用定量模拟、多矿物-流体相互作用定量模拟和多相多组分流体-岩石相互作用定量模拟。今后拟重点开展的研究有:层序地层格架/沉积相带框架下不同成岩体内的流体-岩石相互作用研究,陆相断陷盆地内与深大断裂、断裂输导有关的流体-岩石相互作用研究,煤系地层背景下致密储层中有机酸流体-岩石相互作用研究,咸化湖盆储集层中流体-岩石相互作用研究,以及中、新生界碎屑岩风化壳内流体-岩石相互作用研究等。
Abstract:
Diagenetic body is a geological body formed in the process of burial diagenesis, which has genetic relationship and different scales. Starting from the study of multiscale diagenetic body, the thermodynamic and kinetic conditions for controlling fluid-rock interaction in the diagenetic body were elucidated, and the mechanism of fluid-rock interaction was revealed. Classification scheme of diagenetic body for diagenetic facies as the core, including diagenetic system tract scale, diagenetic system scale, diagenetic facies scale, and diagenetic sub-facies scale, was proposed. The new progress of the above four diagenetic bodies in different scales was summarized. From the point of view of the interaction between single phase/multiphase fluid and single mineral/multi-mineral, the quantitative simulation technology of fluid-rock interaction can be classified as fluid-feldspar interaction, fluid-quartz interaction, fluid-multi-mineral interaction and multiphase multicomponent-fluid interaction quantitative simulations. The study on fluid-rock interaction is suitable for focusing on research issues, such as the geo-body under a stratigraphic sequence framework/sedimentary facies belt framework, the continental rift basin related to deep fault and fault accommodation, the organic acid from tight reservoir in coal-bearing strata, the reservoir in saline lacustrine basin, and the clastic weathering crust in Mesozoic-Cenozoic

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备注/Memo

备注/Memo:
收稿日期:2017-03-17
基金项目:国家科技重大专项项目(2016ZX05027-004-002,2016ZX05031001-001-003);国家自然科学基金项目(41602135);中央高校基本科研业务费专项资金项目(17CX06034)
作者简介:林承焰(1963-),男,福建福清人,教授,博士研究生导师,工学博士,E-mail:lincy@upc.edu.cn。
更新日期/Last Update: 2017-07-28