Coupled Microfracturing and Chemical Weathering of Precambrian Quartzite in the Extremely Humid and Tectonically Active Shillong Plateau, NE India: Implications for In Situ Quartz Weathering and Quartz Silt Production

IF 1.5 4区 地球科学 Q2 GEOLOGY
Journal of Geology Pub Date : 2020-02-13 DOI:10.1086/707326
S. Sensarma, R. V. S. Shimyaphy, T. Chakraborty
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引用次数: 1

Abstract

The origin of quartz silt, the most abundant detrital particle, is controversial. Quartz silt is generally considered to be broken quartz sand, attributed to glacial, eolian, and/or long fluvial transport. In this article, we highlight the origin of in situ quartz silt in deep weathering profiles (≤7 m) over Precambrian quartzite (>92% quartz with or without 6%–8% mica, feldspar-free), a rock known to be resistant to weathering, in the Shillong Plateau (NE India). This region is one of the most tectonically active and the rainiest place on Earth. We discuss, for the first time, detailed field petrographic and microstructural evidence including diverse microfracturing and dissolution morphologies in quartz, from bedrock through saprolite (2–3 m) and nodular zone (NZ; ∼0.5 m) to soil (≤2–5 m), for quartz silt production through coupled mechanical-chemical processes over 3–4 My in the plateau. Progressive size reduction of quartz from medium sand (1.13–1.36 Φ) in bedrock quartzite through fine sand in saprolite (2.55–2.67 Φ) and the NZ (2.12–4.4 Φ) to coarse and medium silt in soil (4–5 Φ), with concomitant increase in clay mineral (≤80%), characterizes the profiles. Quartzite microfracturing, linked to exhumation and/or seismicity, provided pathways for acidic water to attack and promote chemical weathering in quartz, which in turn effected microfracture widening, porosity enhancement, and weakening of quartz in a positive feedback loop. Mica-microbe interactions facilitated fluid acidity, causing Al and Fe mobilization and more clay mineral production, and enhanced corrosive potential for in situ quartz dissolution in feldspar-free quartzite. Coupled brittle disintegration and chemical weathering of even extremely resistant quartz-rich rocks thus contribute toward long-term regolith development and global quartz silt production.
印度东北部极度潮湿和构造活跃的西龙高原前寒武纪石英岩的微压裂和化学风化耦合作用:对原位石英风化和石英粉生成的启示
石英粉土是最丰富的碎屑颗粒,其来源一直存在争议。石英粉土通常被认为是破碎的石英砂,归因于冰川、风成岩和/或长期河流输送。在这篇文章中,我们强调了Shillong高原(印度东北部)前寒武纪石英岩(>92%石英,含或不含6%–8%云母,无长石)深层风化剖面(≤7 m)中原位石英粉土的起源,该岩石是一种已知的抗风化岩石。该地区是地球上构造最活跃、降雨量最大的地区之一。我们首次讨论了详细的野外岩石和微观结构证据,包括石英中的不同微裂缝和溶解形态,从基岩到腐泥土(2-3 m)和结节区(NZ;~0.5 m)到土壤(≤2-5 m),通过高原3-4 My的耦合机械化学过程产生石英粉土。石英从基岩石英岩中的中砂(1.13–1.36Φ),到腐泥土中的细砂(2.55–2.67Φ)和NZ(2.12–4.4Φ),再到土壤中的粗粒和中粒粉土(4–5Φ),随着粘土矿物(≤80%)的增加,粒度逐渐减小,这是剖面的特征。石英岩微裂缝与剥露和/或地震活动有关,为酸性水侵蚀和促进石英的化学风化提供了途径,从而在正反馈回路中影响微裂缝的扩大、孔隙度的增强和石英的弱化。云母-微生物的相互作用促进了流体的酸性,导致铝和铁的迁移以及更多的粘土矿物的产生,并增强了石英在无长石石英岩中原位溶解的腐蚀潜力。因此,即使是极具抵抗力的富含石英的岩石,其脆性崩解和化学风化作用的结合也有助于长期风化层的开发和全球石英粉土的生产。
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
Journal of Geology
Journal of Geology 地学-地质学
CiteScore
3.50
自引率
5.60%
发文量
0
审稿时长
3 months
期刊介绍: One of the oldest journals in geology, The Journal of Geology has since 1893 promoted the systematic philosophical and fundamental study of geology. The Journal publishes original research across a broad range of subfields in geology, including geophysics, geochemistry, sedimentology, geomorphology, petrology, plate tectonics, volcanology, structural geology, mineralogy, and planetary sciences. Many of its articles have wide appeal for geologists, present research of topical relevance, and offer new geological insights through the application of innovative approaches and methods.
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