印度比尔瓦拉超群坦旺岩太古宙碳酸盐沉积物的主要、痕量和稀土元素地球化学:对海水地球化学和沉积环境的影响

IF 1.1 4区 地球科学 Q3 GEOLOGY
Rohit Kumar, Abdul Hameed, Pooja Tiwari, Nandan Kumar, Pankaj Srivastava
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引用次数: 0

摘要

太古宙沉积物的地球化学可能有助于破译地球原始海水化学和沉积环境。本研究以印度拉贾斯坦邦比尔瓦拉超群 Tanwan 组岩石的碳酸盐沉积物为基础,重点介绍了 2.9-2.5 Ga 期间沉积的地球化学演化、氧化还原条件和沉积环境。这些碳酸盐沉积物的岩石学特征和主要元素的变化表明,在这一时期发生了广泛的白云石化。元素比率(如 Mg/Ca、Fe/Al、Fe/Sr 和 Mn/Sr 比率)及其相互关系表明碳酸盐沉淀过程中存在缺氧条件。Ni/Co、V/Cr、V/V + Ni、V/V + Cr 和 Th/U 等对氧化还原敏感的元素比值也充分证明了缺氧的存在,这些元素比值显示了 2.9-2.5 Ga 期间的还原/缺氧沉积环境。后太古宙澳大利亚页岩(PAAS)的归一化异常,如Ce异常、Gd异常和Eu异常,平均值为1-1.48,表明太古宙海水中存在轻微的正异常。这些沉积物中的稀土元素和钇(REY)含量没有显示出明显的污染、混合和蚀变,因为溶解 II(碳酸盐浸出液)的特征是锆含量从 0.015 ppm 到低于检测限(BDL),钍含量为 1 ppm,钪含量为 1.5 ppm,氧化铝含量为 1%。Y/Ho 比率为 26,表明在碳酸盐沉淀过程中输入的碎屑微不足道。Y/Ho 与 Nd 的比率也支持这一论点。Y异常(即 Y/Ho >26)、Gd异常(Gd/Gd*)和La异常(La/La*)证实了在这些主要沉积于新元古代的比尔瓦拉超群碳酸盐岩中保留了缺氧原始海水的特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Major, trace and rare earth element geochemistry of Archaean carbonate sediments of Tanwan group rocks of the Bhilwara supergroup, India: implications for seawater geochemistry and depositional environment

Major, trace and rare earth element geochemistry of Archaean carbonate sediments of Tanwan group rocks of the Bhilwara supergroup, India: implications for seawater geochemistry and depositional environment

Geochemistry of the sediments deposited during the Archaean Era is potentially useful to decipher the Earth’s pristine seawater chemistry and the depositional environment. This study highlights the geochemical evolution, redox conditions, and the sedimentary environment based on carbonate sediments of the Tanwan group rocks, Bhilwara supergroup, Rajasthan, India, deposited during 2.9–2.5 Ga. The petrographic features and variation in major elements of these carbonate sediments indicate extensive dolomitization during this time. The elemental ratios such as Mg/Ca, Fe/Al, Fe/Sr, and Mn/Sr ratios and their mutual relationships suggest anoxic conditions during precipitation of the carbonates. The anoxia is well supported by the redox-sensitive element ratios such as Ni/Co, V/Cr, V/V + Ni, V/V + Cr, and Th/U, which show reducing/anoxic sedimentary environments during 2.9–2.5 Ga. The post-Archaean Australian Shale (PAAS) normalized anomalies, such as Ce anomaly, Gd anomaly, and Eu anomaly, showing average 1–1.48 values, indicate minor positive anomalies in the Archaean seawater. The rare earth elements and yttrium (REY) content in these sediments show no significant contamination, mixing, and alteration because Dissolution II (carbonate leachate) is characterized by Zr from 0.015 ppm to below detection limit (BDL), Th < 1 ppm, Sc < 1.5 ppm, and Al2O3 < 1%. The Y/Ho ratio > 26 represents insignificant detrital input during the precipitation of the carbonates. The Y/Ho ratio versus Nd also supports this contention. The positive anomalies for Y (i.e. Y/Ho > 26), Gd anomaly (Gd/Gd*), and La anomaly (La/La*) confirmed the preservation of anoxic pristine marine seawater signatures in these carbonates of the Bhilwara supergroup that were mainly deposited during the Neoarchaean Era.

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来源期刊
Carbonates and Evaporites
Carbonates and Evaporites 地学-地质学
CiteScore
2.80
自引率
14.30%
发文量
70
审稿时长
3 months
期刊介绍: Established in 1979, the international journal Carbonates and Evaporites provides a forum for the exchange of concepts, research and applications on all aspects of carbonate and evaporite geology. This includes the origin and stratigraphy of carbonate and evaporite rocks and issues unique to these rock types: weathering phenomena, notably karst; engineering and environmental issues; mining and minerals extraction; and caves and permeability. The journal publishes current information in the form of original peer-reviewed articles, invited papers, and reports from meetings, editorials, and book and software reviews. The target audience includes professional geologists, hydrogeologists, engineers, geochemists, and other researchers, libraries, and educational centers.
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