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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Towards an improved understanding of erosion rates and tidal notch development on limestone coasts in the Tropics: 10years of micro- erosion meter measurements, Phang Nga Bay, Thailand
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Towards an improved understanding of erosion rates and tidal notch development on limestone coasts in the Tropics: 10years of micro- erosion meter measurements, Phang Nga Bay, Thailand

机译:为了更好地了解热带地区石灰岩海岸的侵蚀率和潮汐口发展:泰国攀牙湾的微侵蚀仪测量十年

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Knowledge and understanding of shore platform erosion and tidal notch development in the tropics and subtropics relies mainly on short-term studies conducted on recently deposited carbonate rocks, predominantly Holocene and Quaternary reef limestones and aeolianites. This paper presents erosion rates, measured over a 10year period on notches and platforms developed on the Permian, Ratburi limestone at Phang Nga Bay, Thailand. In so doing it contributes to informing a particular knowledge gap in our understanding of the erosion dynamics of shore platform and tidal notch development in the tropics and subtropics - notch erosion rates on relatively hard, ancient limestones measured directly on the rock surface using a micro-erosion meter (MEM) over time periods of a decade or more. The average intertidal erosion rate of 0.231mm/yr is lower than erosion rates measured over 2-3 years on recent, weaker carbonate rocks. Average erosion rates at Phang Nga vary according to location and site and are, in rank order from highest to lowest: Mid-platform (0.324mm/yr)>Notch floor (0.289mm/yr)>Rear notch wall (0.228mm/yr)>Lower platform (0.140mm/yr)>Notch roof (0.107mm/yr) and Supratidal (0.095mm/yr). The micro-relief of the eroding rock surfaces in each of these positions exhibits marked differences that are seemingly associated with differences in dominant physical and bio-erosion processes. The results begin to help inform knowledge of longer term shore platform erosion dynamics, models of marine notch development and have implications for the use of marine notches as indicators of changes in sea level and the duration of past sea levels. Copyright (c) 2014 John Wiley & Sons, Ltd.
机译:对热带和亚热带海岸平台侵蚀和潮汐口发展的认识和理解主要取决于对最近沉积的碳酸盐岩,主要是全新世和第四纪的石灰岩和风成岩进行的短期研究。本文介绍了侵蚀速率,该速率是在泰国攀牙湾二叠纪,Ratburi石灰岩上开发的凹口和平台上进行了为期10年的测量。这样做有助于在了解热带和亚热带海岸平台侵蚀动力学和潮汐缺口发展过程中了解一个特定的知识鸿沟-使用微孔直接在岩石表面直接测量相对坚硬的古老石灰石的缺口侵蚀率腐蚀计(MEM)在十年或更长时间内。平均潮间带侵蚀速率为0.231毫米/年,低于最近2-3年对较弱的碳酸盐岩的侵蚀速率。攀牙的平均侵蚀率因位置和地点而异,从高到低的等级顺序为:中平台(0.324mm /年)>缺口层(0.289mm /年)>缺口后壁(0.228mm /年) )>下平台(0.140mm /年)>槽形屋顶(0.107mm /年)和Supratidal(0.095mm /年)。在这些位置的每一个中,侵蚀岩石表面的微浮雕都表现出明显的差异,这似乎与主要的物理和生物侵蚀过程的差异有关。研究结果开始帮助人们了解长期的岸台侵蚀动力学,海洋缺口发展模型,并且对使用海洋缺口作为海平面变化和过去海平面持续时间的指标具有影响。版权所有(c)2014 John Wiley&Sons,Ltd.

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