How does the burial rate control the diagenesis of sandstone? Insights from a diagenetic physical simulation experiment

IF 3.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Chemical Geology Pub Date : 2024-04-30 DOI:10.1016/j.chemgeo.2024.122122
Sirui Chen , Benzhong Xian , Youliang Ji , Jiaqi Li , Naveed Ur Rahman , Rongheng Tian , Pengyu Wang
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Abstract

The study conducted physical simulation experiments on sandstone samples from the Junggar Basin to investigate how burial rates influence sandstone diagenesis and reservoir quality. Results show that the mechanical compaction under a negative burial rate (tectonic uplift) almost stops to destroy the sandstone reservoir space, the capacity of fluid seepage is the strongest and the sandstone tends to develop ‘weak compaction–strong dissolution’ diagenetic facies. For positive burial rates, sandstones with a low burial rate tend to develop ‘medium compaction–medium dissolution’ diagenetic facies; sandstones at a medium burial rate easily form ‘strong compaction–weak dissolution’ diagenetic facies, and sandstones at a high burial rate tend to develop ‘weak compaction–weak dissolution’ diagenetic facies. Experimental results indicate that the compaction strength and damage to sandstone reservoirs may not consistently rise with the burial rate. Faster burial rates do not always intensify compaction; the degree of compaction depends on fluid overpressure. If the increase in burial rate does not induce the fluid overpressure in sandstones, the burial rate is higher and the destruction degree of primary pores caused by mechanical compaction is greater; mechanical compaction also simultaneously causes the diagenetic system to be more closed and the dissolution to be weaker. If the increase in burial rate can induce the fluid overpressure in sandstones, the burial rate is higher, the inhibition of mechanical compaction by fluid overpressure is more pronounced. However, fluid overpressure also strengthens the closure of the diagenetic system, hindering the injection of external acidic fluids into the sandstone, which is not conducive to dissolution. Overall, low burial rates with normal pressure favour secondary pore development, high burial rates with overpressure preserve primary pores, while medium burial rates with normal pressure are unfavourable for primary and secondary pores.

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埋藏率如何控制砂岩的成岩作用?成岩物理模拟实验的启示
该研究对准噶尔盆地的砂岩样本进行了物理模拟实验,以研究埋藏率如何影响砂岩成因和储层质量。结果表明,在负埋藏率(构造隆起)条件下,机械压实几乎停止破坏砂岩储层空间,流体渗流能力最强,砂岩倾向于发育 "弱压实-强溶蚀 "成因面。对于正埋藏率,低埋藏率砂岩倾向于形成 "中等压实-中等溶解 "成因面;中等埋藏率砂岩容易形成 "强压实-弱溶解 "成因面;高埋藏率砂岩倾向于形成 "弱压实-弱溶解 "成因面。实验结果表明,砂岩储层的压实强度和破坏程度可能不会随着埋藏率的增加而持续上升。较快的埋藏率并不总是会加强压实;压实程度取决于流体超压。如果埋藏率的提高不能引起砂岩中的流体超压,那么埋藏率越高,机械压实对原生孔隙的破坏程度就越大;机械压实也同时会使成岩体系更加封闭,溶蚀作用减弱。如果埋藏率的提高能引起砂岩中的流体超压,则埋藏率越高,流体超压对机械压实的抑制作用越明显。但流体超压也会加强成岩体系的封闭性,阻碍外部酸性流体注入砂岩,不利于溶解。总体而言,常压下的低埋藏率有利于次生孔隙发育,超压下的高埋藏率可保留原生孔隙,而常压下的中等埋藏率则不利于原生和次生孔隙。
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来源期刊
Chemical Geology
Chemical Geology 地学-地球化学与地球物理
CiteScore
7.20
自引率
10.30%
发文量
374
审稿时长
3.6 months
期刊介绍: Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry. The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry. Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry. The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.
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