~530 Ma古dem时空插值量化地球撞击坑剥蚀

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
J. Aswathi , S. James , S. Keerthy , A. Rajaneesh , V.R. Rani , K.S. Sajinkumar , Thomas Oommen , R.B. Binoj Kumar
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引用次数: 0

摘要

侵蚀和风化是控制地貌演化强度和模式的两个外生过程。根据以前的研究,在地质历史中观察到的不同侵蚀速率取决于平均地形(形态)、气候、岩性和时间等因素。陨石撞击坑具有独特的地貌特征,其特征既有负面起伏特征(碗状凹陷),也有正面特征(如凸起的边缘;此外,中央高架区域为复杂的陨石坑)。这使它们成为研究侵蚀和沉积的合适形态特征。这项研究估计了印度西部拉姆加尔陨石坑的长期侵蚀,这个陨石坑在其形态和侵蚀速率上存在争议。这项研究使用了古数字海拔模型(古dem),重建了⁓528 Ma (Ramgarh形成的潜在上年龄)的陨石坑形态,以及先前建立的模型,并进行了适当的修改,以量化从最后阶段到现在的侵蚀。对弹丸的类型及其直径、体积等物理特性进行了估计。通过GPlates(基于gis的古重建模型)重建陨石坑的古位置,然后重建两个年龄限制(528 Ma和395 Ma)的瞬态和最终陨石坑形态(包括陨石坑直径和真实深度、边缘高度和近端喷出物厚度等参数)。陨石坑的间歇性形态是用数学方程来描述随时间变化的顺序的。陨石坑的侵蚀,按累积体积量化,在0.41和0.58 km3之间。这个范围是基于与两个不同的最终火山口边缘高度(数学推导)有关的四个条件以及两个年龄限制。总的来说,这项研究为Ramgarh陨石坑的长期形态演化提供了有价值的见解,并有助于了解陨石坑的侵蚀过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Spatio-temporal interpolation of ~530 Ma paleo-DEM to quantify denudation of a terrestrial impact crater

Spatio-temporal interpolation of ~530 Ma paleo-DEM to quantify denudation of a terrestrial impact crater
Erosion and weathering are two of the several exogenic processes that control the intensity and patterns of landform evolution. Based on previous studies, the varied erosion rates observed in the geological past depends on factors like mean relief (morphology), climate, lithology, and time. Meteorite impact craters have unique geomorphic features, being characterized by both negative relief features (the bowl-shaped depression) and positive features (such as elevated rims; additionally, central elevated areas for complex craters). This makes them a suitable morphologic feature to study both erosion and deposition. This study estimates the long-term erosion of Ramgarh crater in western India, a crater debated on its morphology and erosion rates. This study uses a paleo-digital elevation model (paleo-DEM), a reconstruction of the crater morphology at ⁓528 Ma- the potential upper age of formation of Ramgarh, along with previously established models with suitable modifications to quantify erosion from the final stage to the present day. The type of projectile and its physical characteristics such as diameter and volume were also estimated. Reconstruction of the crater's paleo-position was achieved through GPlates (a GIS-based paleo-reconstruction model), followed by recreating the transient and final crater morphology (including parameters such as crater diameter and true depth, rim height, and thickness of proximal ejecta) for two age limits (528 Ma and 395 Ma). The intermittent morphology of the crater was generated using mathematical equations to depict the sequence of changes through time. The erosion of the crater, quantified in terms of cumulative volume, is between 0.41 and 0.58 km3. This range is based on four conditions pertaining to two different final crater rim heights (mathematically derived) as well as two age limits. Overall, this study provides valuable insights into the long-term morphological evolution of Ramgarh crater and contributes to the understanding of impact crater's erosion processes.
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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