A new type of dolomicrite envelope formed in Oligocene lacustrine sediments and its significance for preserving porosity, Bohai Bay Basin, North China

IF 2.7 2区 地球科学 Q1 GEOLOGY
Caineng Mu , Xiaobo Huang , Liya Da , Anqing Chen , James G. Ogg , Huan Lu , Yuzhu Ge , Jian Luo , Siyu Xiong , Haiyang Cao , Mingcai Hou
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Abstract

Micrite envelopes are common early diagenetic features in marine carbonate grains. Most case studies of micrite envelopes focus on those with calcium-carbonate compositions. This paper documents a new type of lacustrine dolomicrite envelopes, coating both terrigenous grains and bioclasts, which developed in the upper Shahejia Formation of early Oligocene age in the middle of the Bohai Bay Basin. These dolomicrite envelopes on grains in a lacustrine mixed sedimentary environment are puzzling for their formation and linkage with the porosity preservation of porosity among grains. We investigate the microstructure and formation mechanism of these dolomicrite envelopes that coat grains through the study of the mineralogy, petrology and porosity characteristics. These studies show that there are two occurrences of the dolomicrite envelopes, i.e., coating on detrital grains and coating on carbonate grains, with a multi-layer microstructure. A potential two stage model to interpret the formation of dolomicrite envelopes incorporates an initial illite coating followed by dolomite encrustation. The illite coating played an important role in the precipitation of the dolomite. Post-envelope diagenetic processes include sparry cementation and destructive dissolution. The quantitative content of dolomicrite envelopes positively correlates with the preserved porosity, which suggests that their formation contributed to resisting compaction and protecting porosity among grains. Indeed, the dolomicrite envelopes appear to have aided in maintaining a kind of extremely high-quality reservoir for hydrocarbon exploration within the Shahejia Formation of the Bohai Bay Basin. In addition, the coating film seems to be conducive to the exchange of anions, thereby resulting in the dissolution of interior feldspar-, bioclast- or ooid-grains. In summary the Shahejia Formation of the Bohai Bay Basin provides a new type of dolomicrite envelope on grains in a lacustrine setting.

华北渤海湾盆地渐新世湖相沉积物中形成的一种新型白云岩包体及其对保存孔隙度的意义
微晶包络是海洋碳酸盐颗粒中常见的早期成岩特征。大多数关于微晶岩包层的案例研究都集中在碳酸钙成分的微晶岩包层上。本文记录了在渤海湾盆地中部早更新世上部沙河家地层中发育的一种新型湖相白云母包体,它既包裹着陆生颗粒,也包裹着生物碎屑。在湖相混合沉积环境中,这些包覆在颗粒上的白云母包层的形成及其与颗粒间孔隙度保存的联系令人费解。我们通过对矿物学、岩石学和孔隙度特征的研究,调查了这些包裹在颗粒上的白云母包体的微观结构和形成机制。这些研究表明,白云母包体有两种情况,即包裹在脱落晶粒上和包裹在碳酸盐晶粒上,具有多层微观结构。解释白云母包层形成的潜在两阶段模型包括最初的伊利石包层和随后的白云石包层。伊利石包层在白云石的沉淀过程中发挥了重要作用。包壳后成岩过程包括疏松胶结和破坏性溶解。白云岩包体的数量含量与保存的孔隙度呈正相关,这表明包体的形成有助于抵抗压实和保护晶粒间的孔隙度。事实上,白云母包膜似乎有助于在渤海湾盆地沙河家地层中维持一种极优质的油气勘探储层。此外,包膜似乎有利于阴离子的交换,从而导致内部长石粒、生物碎屑岩粒或类卵石粒的溶解。总之,渤海湾盆地的沙河家地层提供了一种新类型的湖积环境中晶粒上的白云母包膜。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Sedimentary Geology
Sedimentary Geology 地学-地质学
CiteScore
5.10
自引率
7.10%
发文量
133
审稿时长
32 days
期刊介绍: Sedimentary Geology is a journal that rapidly publishes high quality, original research and review papers that cover all aspects of sediments and sedimentary rocks at all spatial and temporal scales. Submitted papers must make a significant contribution to the field of study and must place the research in a broad context, so that it is of interest to the diverse, international readership of the journal. Papers that are largely descriptive in nature, of limited scope or local geographical significance, or based on limited data will not be considered for publication.
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