Dongya Zhu , Quanyou Liu , Xiaowei Huang , Qingqiang Meng , Jingbin Wang , Pengpeng Li , Zhijun Jin
{"title":"Large-scale accumulation of abiotic gases associated with subduction and volcanic activities in rift basins in eastern China","authors":"Dongya Zhu , Quanyou Liu , Xiaowei Huang , Qingqiang Meng , Jingbin Wang , Pengpeng Li , Zhijun Jin","doi":"10.1016/j.orggeochem.2024.104900","DOIUrl":null,"url":null,"abstract":"<div><div>A series of large-scale abiotic gas reservoirs have been discovered in a few rift basins in eastern China. However, the compositions of the abiotic gases in each gas reservoir differ significantly, dominated by CO<sub>2</sub> or CH<sub>4</sub>. This study aims to explore the factors controlling the large-scale generation and accumulation of different types of abiotic gases in the reservoirs. CO<sub>2</sub> is the major component of the abiotic gases in the Huangqiao, Huagou, and Pingfangwang reservoirs, exceeding 60 % up to 95 % and the δ<sup>13</sup>C<sub>CO2</sub> values are generally greater than −8‰. CH<sub>4</sub> is the major component in the Qingshen and Songnan reservoirs with content up to 94.98 %. The δ<sup>13</sup>C<sub>CH4</sub> values are commonly greater than −30 ‰ (up to −16.8 ‰) and the alkanes exhibit a reverse sequence (δ<sup>13</sup>C<sub>CH4</sub> > δ<sup>13</sup>C<sub>C2H6</sub> > δ<sup>13</sup>C<sub>C3H8</sub> > δ<sup>13</sup>C<sub>C4H10</sub>). Most of the <sup>3</sup>He/<sup>4</sup>He ratios of the reservoirs are commonly greater than 1 Ra. The carbon isotope values and <sup>3</sup>He/<sup>4</sup>He ratios indicate that most of the gas components (CO<sub>2</sub> or CH<sub>4</sub>) are abiotic. The abiotic CO<sub>2</sub> is associated with mantle-degassing, and abiotic CH<sub>4</sub> is mantle-derived and/or attributed to Fischer-Tropsch (FT) reactions. The ratios of Fe<sup>3+</sup>/∑Fe of the basalt near the Huangqiao reservoir are higher than those near the Qingshen and Songnan reservoirs, suggesting the relatively oxygen-fugacity controls the major component of the abiotic gases. The northwestward subduction of the western Pacific Plate, starting from the Japan Trench, triggered extensive magmatic and volcanic activities, resulting in the release and accumulation of abiotic gases in the rift basins. The variation in oxygen fugacity associated with oxidizing materials (e.g., iron and manganese oxides) and carbonate and sulfate sediments carried by the subducted plate determined the presence of abiotic CO<sub>2</sub> or CH<sub>4</sub>. As the subduction slab continues moving forward beneath the continental plate, the influence of high-oxygen-fugacity materials gradually decreases, causing the abiotic gases to transition from CO<sub>2</sub> to CH<sub>4</sub>. The Huangqiao, Huagou, Pingfangwang, Songnan, and Qingshen gas reservoirs are located farther away from the subducting slab, which explains the gradual shift in the abiotic component in these reservoirs. In general, the majority of the abiotic gases are released from deep faults and magmatic eruptions. Therefore, we conclude that the abiotic gas reservoirs are located near deep faults and igneous rocks.</div></div>","PeriodicalId":400,"journal":{"name":"Organic Geochemistry","volume":"200 ","pages":"Article 104900"},"PeriodicalIF":2.6000,"publicationDate":"2025-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Organic Geochemistry","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0146638024001657","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
A series of large-scale abiotic gas reservoirs have been discovered in a few rift basins in eastern China. However, the compositions of the abiotic gases in each gas reservoir differ significantly, dominated by CO2 or CH4. This study aims to explore the factors controlling the large-scale generation and accumulation of different types of abiotic gases in the reservoirs. CO2 is the major component of the abiotic gases in the Huangqiao, Huagou, and Pingfangwang reservoirs, exceeding 60 % up to 95 % and the δ13CCO2 values are generally greater than −8‰. CH4 is the major component in the Qingshen and Songnan reservoirs with content up to 94.98 %. The δ13CCH4 values are commonly greater than −30 ‰ (up to −16.8 ‰) and the alkanes exhibit a reverse sequence (δ13CCH4 > δ13CC2H6 > δ13CC3H8 > δ13CC4H10). Most of the 3He/4He ratios of the reservoirs are commonly greater than 1 Ra. The carbon isotope values and 3He/4He ratios indicate that most of the gas components (CO2 or CH4) are abiotic. The abiotic CO2 is associated with mantle-degassing, and abiotic CH4 is mantle-derived and/or attributed to Fischer-Tropsch (FT) reactions. The ratios of Fe3+/∑Fe of the basalt near the Huangqiao reservoir are higher than those near the Qingshen and Songnan reservoirs, suggesting the relatively oxygen-fugacity controls the major component of the abiotic gases. The northwestward subduction of the western Pacific Plate, starting from the Japan Trench, triggered extensive magmatic and volcanic activities, resulting in the release and accumulation of abiotic gases in the rift basins. The variation in oxygen fugacity associated with oxidizing materials (e.g., iron and manganese oxides) and carbonate and sulfate sediments carried by the subducted plate determined the presence of abiotic CO2 or CH4. As the subduction slab continues moving forward beneath the continental plate, the influence of high-oxygen-fugacity materials gradually decreases, causing the abiotic gases to transition from CO2 to CH4. The Huangqiao, Huagou, Pingfangwang, Songnan, and Qingshen gas reservoirs are located farther away from the subducting slab, which explains the gradual shift in the abiotic component in these reservoirs. In general, the majority of the abiotic gases are released from deep faults and magmatic eruptions. Therefore, we conclude that the abiotic gas reservoirs are located near deep faults and igneous rocks.
期刊介绍:
Organic Geochemistry serves as the only dedicated medium for the publication of peer-reviewed research on all phases of geochemistry in which organic compounds play a major role. The Editors welcome contributions covering a wide spectrum of subjects in the geosciences broadly based on organic chemistry (including molecular and isotopic geochemistry), and involving geology, biogeochemistry, environmental geochemistry, chemical oceanography and hydrology.
The scope of the journal includes research involving petroleum (including natural gas), coal, organic matter in the aqueous environment and recent sediments, organic-rich rocks and soils and the role of organics in the geochemical cycling of the elements.
Sedimentological, paleontological and organic petrographic studies will also be considered for publication, provided that they are geochemically oriented. Papers cover the full range of research activities in organic geochemistry, and include comprehensive review articles, technical communications, discussion/reply correspondence and short technical notes. Peer-reviews organised through three Chief Editors and a staff of Associate Editors, are conducted by well known, respected scientists from academia, government and industry. The journal also publishes reviews of books, announcements of important conferences and meetings and other matters of direct interest to the organic geochemical community.