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首页> 外文期刊>Journal of South American earth sciences >Landscape evolution of the graben of Puerto Vallarta (west-central Mexico) using the analysis of landforms and stream long profiles
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Landscape evolution of the graben of Puerto Vallarta (west-central Mexico) using the analysis of landforms and stream long profiles

机译:使用地貌和河流长剖面分析对巴亚尔塔港(墨西哥中西部)en藜的景观演变

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The analysis of landforms and stream long profiles are useful tools that can provide information about the tectonic activity in the landscape. The west-central portion of Mexico is a region that is mostly dominated by an extensional tectonics initiated in the Miocene and continuing in the Quaternary, where there has also been a vast emission of volcanic products. Of particular importance is the graben of Puerto Vallarta which was formed during the extensional activity that opened the Gulf of California in the Miocene. Nevertheless, the geomorphology and landscape evolution of this structure has not been studied in detail. Here I present a study of the rivers, landforms and topography of Puerto Vallarta graben in order to assess its evolution, focusing on the evidences of its initial phase of formation. The geomorphological map elaborated in this study reveals the presence of lava flows and volcanic structures in the eastern sector of the graben. Here it is proposed that this volcanism occurred during the formation of the graben in the Miocene, nevertheless, radiometric dating of lavas is still required to determine the precise timing of this event. Analysis of stream long profiles confirms that knickpoints are propagating in the fluvial network at a rate of similar to 0.07 to similar to 0.7 mm yr(-1) and these were probably triggered by a drop in the base-level of rivers during the graben formation. The rates of knickpoint retreat in the graben of Puerto Vallarta are slightly lower than those observed in other recent (Quaternary) tectonic areas, however, the migration rates of the graben of Puerto Vallarta were probably higher at the onset of the faulting. Here the analysis of landforms and stream long profiles were useful to elucidate one part of the evolution of the graben of Puerto Vallarta. This study emphasizes the importance of incorporating the tectonic geomorphology in future studies of the extensional zones of west-central Mexico. (C) 2016 Elsevier Ltd. All rights reserved.
机译:地貌分析和河流长剖面分析是有用的工具,可以提供有关景观中构造活动的信息。墨西哥的中西部地区是一个主要由中新世开始并一直延续到第四纪的伸展构造所控制的地区,那里也散发着大量的火山产物。尤为重要的是瓦拉塔港(Puerto Vallarta)的grab起,它是在中新世开启加利福尼亚湾扩张活动期间形成的。然而,尚未对该结构的地貌和景观演化进行详细研究。在这里,我将对巴亚尔塔港grab的河流,地貌和地形进行研究,以评估其演变过程,重点是其形成初期的证据。这项研究详细阐述的地貌图揭示了在the石东部地区存在熔岩流和火山结构。在此提出,这种火山作用是在中新世the陷形成期间发生的,尽管如此,仍需要对熔岩进行放射线测年,以确定这一事件的确切时间。对河流长剖面的分析证实,拐点在河流网络中的传播速率约为0.07至0.7 mm yr(-1),这很可能是由于grab流形成过程中河流基础水平的下降而触发的。 。巴亚尔塔港the陷的拐点退缩率略低于其他最近的(第四纪)构造区域,但是,巴库尔塔港grab陷的迁移率在断层发生时可能更高。在这里,对地貌和河流长剖面的分析对于阐明巴亚尔塔港grab斗演变的一部分很有用。这项研究强调了在未来墨西哥中西部延伸区研究中纳入构造地貌的重要性。 (C)2016 Elsevier Ltd.保留所有权利。

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