前弧盆地:墨西哥下加利福尼亚马格达莱纳陆架地下特征的地震反射剖面解释

A Mastache-RománEdgar, González-Escobar Mario
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摘要

在墨西哥下加利福尼亚州马格达莱纳陆架(Magdalena Shelf, Baja California)一个包含弧前盆地的区域收集了8条二维地震反射剖面,提供了该盆地断层和地震反射体的空间视图。构造了2个小型不对称盆地;ToscoAbreojos和San Lázaro受Tosco-Abreojos和Santa Margarita-San Lázaro断层控制。这些断裂容纳了陆架内很大一部分的张拉应力,控制了陆架的水深,并在西段表现出很大的变形。地震水平表明,San Lazaro盆地的沉积中心深度为~4 km,而ToscoAbreojos盆地的沉积中心深度约为~5.5 km,在这些深度存在一个漫反射体,被认为是声学基底。圣玛格丽塔断层存在于圣玛格丽塔岛和马格达莱纳岛,向西北延伸,然后停止呈现以圣拉扎罗断层为代表的地形,这与该地区最近报道的地震活动有关。在这一地区也观察到以前由其他工作报告的在该地区南部观察到的反射体。然而,北西向有新的反射体,它们填补了两个盆地的空间,总共占据了8个地震地层单元。整个将新近系层序与填满弧前盆地的古新世-始新世层序分开的区域都存在不整合。在不整合面下方,有一个巨大的中新世沉积物包。该构造高度与沿Magdalena陆架向SE-NW方向延伸的俯冲杂岩相对应,被认为是蛇绿岩的声学基底。这种构造高度可能与位于下加利福尼亚州中部的上拉古尼塔斯有关,那里也存在蛇绿岩。但马格达莱纳冰架比上拉古尼塔斯冰架更晚,因为这里的岩石更年轻。从获得的结果来看,圣玛格丽塔断层应该被考虑用于未来的风险研究,因为它是构造活跃的,它的路径经过人口中心附近,如圣卡洛斯港。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Forearc Basin: Characteristics of the Subsurface in Magdalena Shelf, Baja California, Mexico, from the Interpretation of Seismic-Reflection Profiles
Eight seismic reflection profiles, two dimensions, were collected in a sector of the Magdalena Shelf, Baja California, Mexico, which contains a forearc basin, providing a spatial view of faults and seismic reflectors in this basin. Two small asymmetric basins were configured; ToscoAbreojos and San Lázaro controlled by the Tosco-Abreojos and Santa Margarita-San Lázaro Faults. These faults accommodate a great part of the transtensional stress in the shelf and control the bathymetry and show great deformation in the western sector. Seismic horizons illustrate that the depocenter of the San Lazaro basin reaches depths of ~4 km, while the ToscoAbreojos account reaches depths of around ~5.5 km, being present at these depths a diffuse reflector that is considered the acoustic basement. Santa Margarita fault is present in the Santa Margarita and Magdalena islands, extending northwest, then stop presenting its relief represented by the San Lazaro fault, which is associated with the seismic activity resent reported for the region. Reflectors observed to the south of the region, previously reported by other works, were also observed in this area. However, there are new reflectors to the NW, which fill the spaces of both basins, taking a total of eight seismostratigraphic units. Unconformity is present throughout the region that separates the Neogene sequence from the PaleoceneEocene sequence that fills the forearc basin. Below the unconformity, there is a huge packet of Miocene sediments. Structural height corresponding to the subduction complex that extends in the SE-NW direction along the Magdalena Shelf is present, which is considered as the acoustic basement and is attributed to the ophiolite rocks. This structural height can be related to the Alto Lagunitas, located in the central part of Baja California, where an ophiolite rock is also present. But Magdalena Shelf is more recent than the Alto Lagunitas since the said rocks in this place are younger arch. From the results obtained, Santa Margarita Fault should be considered for future risk studies, since it is tectonically active and its path passes near population centers, such as Puerto San Carlos.
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