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Understanding the Origin of Patterned Silica Diagenetic Reaction Fronts

Understanding the Origin of Patterned Silica Diagenetic Reaction Fronts
了解图案化二氧化硅成岩反应前沿的起源
批准号:
NE/G008418/1
负责人:
Richard Davies
金额:
$9.09万
依托单位:
依托单位国家:
英国
项目类别:
Research Grant
财政年份:
2009
资助国家:
英国
项目状态:
已结题
起止时间:
2009 至 --

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中文摘要
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英文摘要
A chemical reaction boundary is a layer that forms between the initial chemical reactants and final products of a reaction. As the reaction develops the boundary propagates through a chemical mixture. Reaction boundaries have been documented at atomic (nanometer) scale in the laboratory upto metre-scale in sedimentary rocks. They form patterns and patterned reaction boundaries and the processes by which they form are widely studied, since they are found in chemical, biological and geological systems. Chemical processes are very important in changing sediment into rock and for driving fluids out of sediment. Most studies involve looking at how chemical boundaries form at a centimentre scale - but we have identified patterned reaction boundaries at kilometre-scale in sedimentary rocks and want to find out how they form. This has not been attempted before. We have started to document the largest scale chemical reaction boundaries yet to be seen on the globe. They form patterns which consist of cell or ridge-type networks over 10s of square kilometres. The cells are in 50-200 m in height and up to 2.7 km across. The development of the reaction fronts and the patterns are linked to a host of other geological phenomena and the reaction fronts appear to be a fundamental aspect of sedimentary basin evolution. We have three theories as to how the patterns form, this proposal would allow us to refine where exactly IODP borehole should be positioned to find out which - if any - of our theories is correct. Our work can be divided into two parts: 1. We would analyse seismic reflection datasets provided by the oil and gas industry and through a partnership with StatoilHydro we would establish where IODP boreholes should be located. This research would result in the submission of pre- and full-IODP drilling proposals. 2. The data would allow us to evaluate the risk of encoutering shallow gas or hydrocarbons as well as the chances of slope instability. We would compile a comprehensive assessment of this, therefore our IODP proposal would not require any additional and costly data collection.
期刊论文(3)
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会议论文
Influence of pore water chemistry on silica diagenesis: evidence from the interaction of diagenetic reaction zones with polygonal fault systems
孔隙水化学对二氧化硅成岩作用的影响:成岩反应带与多边形断层系统相互作用的证据
DOI: 10.1144/0016-76492009-049
发表时间: 2010
期刊: Journal of the Geological Society
影响因子: 2.7
作者: [Ireland M]
通讯作者: Ireland M
Economics Observatory Phase 2
  • 批准号:
    ES/X008304/1
  • 项目类别:
    Research Grant
  • 资助金额:
    $155.22万
  • 财政年份:
    2023
  • 负责人:
    Richard Davies
  • 依托单位:
Economics Observatory
  • 批准号:
    ES/V013742/1
  • 项目类别:
    Research Grant
  • 资助金额:
    $122.93万
  • 财政年份:
    2020
  • 负责人:
    Richard Davies
  • 依托单位:
ESRC RCUK Innovation Fellowships
Challenge 1: Assessing and Monitoring the UK Shale Gas Landscape (UKSGL)
  • 批准号:
    NE/R017492/1
  • 项目类别:
    Research Grant
  • 资助金额:
    $152.2万
  • 财政年份:
    2018
  • 负责人:
    Richard Davies
  • 依托单位:
国内基金
海外基金
Lagrangian origin of geometric approaches to scattering amplitudes
  • 批准号:
    24ZR1450600
  • 项目类别:
    省市级项目
  • 资助金额:
    --
  • 批准年份:
    2024
  • 负责人:
    ALEXANDER OCHIROV
  • 依托单位: