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Analysis of a Travertine System Controlled by the Transpressional Activity of the Alhama De Murcia Fault: the Carraclaca Site, Eastern Betic Cordillera, Spain

Frontiers in Earth Science(2023)

Univ Autonoma Madrid | Univ Complutense Madrid | Ctr Invest Energet

Cited 3|Views8
Abstract
Continental carbonates, such as travertines and tufas, formed from CO2-rich groundwater degassing as it emerges at the Earth’s surface, are often associated with major crustal-scale faults. The Carraclaca site, in the Lorca-Totana section of the Alhama de Murcia Fault, Spain, presents a complex geomorphological landscape controlled by active tectonics. The geology here records the interaction between Quaternary alluvial fans, travertines, and a pop-up structure developed in a transpressional section of the fault. The Alhama de Murcia Fault is an 80 km long left-lateral strike-slip fault that is one of the main seismogenic structures in the Iberian Peninsula. In this work, we examined the relation between travertine precipitation in the Carraclaca site and the tectonic activity of this fault zone through morphological and geochemical studies. The δ13C and δ18O isotopic signals indicate that the carbonate deposits are hydrothermal. In addition, the 87Sr/86Sr ratios in the samples suggest subsurface fluid interaction with the Miocene sediments and the Alpujárride basement, located below the alluvial deposits. Tectonic activity in the Alhama de Murcia Fault might generate the opening of deep water circulation in the crust every time a seismic event occurs, giving rise to hydrothermally derived carbonates precipitation. Deep waters rise and reach the surface interacting with meteoric waters, resulting in travertine formation. Therefore, the Carraclaca carbonate deposits study can inform us about the seismogenic cycle of the fault in the Lorca-Totana section.
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travertine,stable isotopes,paleoseismometer,Alhama de Murcia fault,transpressional fault,geochemistry
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要点】:本文通过形态学和地球化学研究,分析了西班牙阿尔哈马德穆尔西亚断层活动对卡拉卡拉地区钙华系统形成的影响,揭示了断层活动与钙华沉淀之间的联系。

方法】:采用δ13C和δ18O同位素分析以及87Sr/86Sr比值测定,研究钙华沉积的来源和形成条件。

实验】:在卡拉卡拉地区进行地质调查和采样,使用的数据集包括δ13C、δ18O和87Sr/86Sr同位素比值,得出钙华沉积是热液成因,并与断层活动密切相关。