与美国中部盆地和山脉省构造史相关的中新世中晚期次新世岩浆形成过程

L. Hose, V. Polyak, Harvey DuChene, J. D. Powell, L. Melim, Gretchen M. Baker, Donald Davis, Y. Asmerom
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摘要

2022 年 5 月至 2023 年 10 月期间,研究人员对内华达州白松县 25 个显示下新世成岩证据的洞穴进行了研究。研究结果表明,盆地和山脉省中部是一个主要的低成洞穴区,其岩浆生成可追溯到中新世。迄今为止获得的洞穴乳状岩U-Pb放射性测定年代涵盖的时间跨度很大,从14Ma到2Ma不等。蛇岭地层在大约 22 Ma 之前的构造剪切可能括进了岩浆形成的最大年龄。因此,岩浆形成开始于 22-14 Ma 之间,早于晚中新世的大部分盆地和山脉伸展构造运动。主要由于铅污染,很难获得该地区常见猛犸象的可靠年代。整个地区的铅含量都很高,这很可能是由于与地壳有关的矿化流体造成的。虽然对 11 个哺乳动物样本(来自 10 个洞穴)进行了铀-铅测年可行性评估,但其中 5 个样本的铅含量过高,无法进行分析。这些洞穴的下生特征包括乳状液、倾斜叶片、气泡轨迹、冲天炉、天花板通风口/管、地板通风口、酸性湖盆、假扇贝(尖顶)和骨架(巨型尖顶)。在这些洞穴中,一个新发现的共同特征是广泛的二次沉积物,这些沉积物是淤泥大小的方解石和石英颗粒的复杂混合物。一些石英颗粒有方解石过度生长,表明是自生的。我们将这些岩石化且多孔的沉积物命名为 "方解石-粉砂岩"。硫酸成岩(SAS)只在雷曼洞穴这一个洞穴中得到了明确的证实,但至少在其他四个研究地点(老曼斯洞穴、大教堂洞穴、#041709-NS-012 和 #LC01 洞穴)都有强烈的怀疑。然而,这些低成因洞穴年代久远,很可能经历了气候和地表地貌的变化,导致表生地下水的广泛改变。证明 SAS 过程的具体证据可能已被后来的表生活动清除或覆盖。
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Mid- to Late-Miocene hypogene speleogenesis tied to the tectonic history of the central Basin and Range province, USA
Twenty-five caves displaying evidence of hypogene speleogenesis in White Pine County, Nevada, were studied between May 2022 and October 2023. Results demonstrate that the central Basin and Range Province is a major hypogenic cave region with speleogenesis dating back to the Middle Miocene. The U-Pb radiometric dates of cave mammillaries obtained so far cover a wide span of time, ranging between 14 Ma to 2 Ma. Tectonic shearing along the Snake Range Décollement up to about 22 Ma probably brackets the maximum age of speleogenesis. Thus, speleogenesis began between 22-14 Ma, which predates most of the Basin and Range extensional tectonism of the Late Miocene. Robust dates for the common mammillaries in the region have been hard to obtain mostly due to Pb contamination. There are elevated levels of Pb throughout the area, likely due to mineralized fluids associated with the décollement. While 11 mammillary samples (from 10 caves) have been assessed for U-Pb dating viability, five contained too much Pb for analysis. Hypogenic features in these caves include mammillaries, tilted folia, bubble trails, cupolas, ceiling vents/tubes, floor vents, acid lake basins, pseudoscallops (cusps), and boneyard (megacusps). A common and newly identified feature of these caves is extensive secondary deposits of a complex mixture with silt-sized calcite and quartz grains. Some quartz grains have calcite overgrowths, suggesting authigenic growth. We named these lithified, and very porous, deposits “calc-siltite”. Sulfuric acid speleogenesis (SAS) has been clearly demonstrated in only one cave, Lehman Caves, but is strongly suspected in at least four other study sites (Old Mans, Cathedral, #041709-NS-012, and #LC01 caves). However, the great antiquity of these hypogenic caves means that they have probably experienced climatic and surface geomorphologic changes resulting in extensive alterations by epigenic groundwater. The evidence specific to demonstrating SAS processes may have been removed or covered by later epigenic activities.
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