巽他海沟的爪哇和苏门答腊部分:由GMT分析和可视化的地貌和地球物理环境

Q4 Social Sciences
Polina Lemenkova
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引用次数: 5

摘要

本文讨论了巽他海沟的地貌,巽他海沟位于印度洋东部,沿着印度尼西亚群岛的苏门答腊岛和爪哇岛。分析了两段海沟的深度差异和坡度变化:爪哇南部样带(108.8?10.10吗?S - 113.0?东经10.75°S)和北苏门答腊样带(东经97.5°S)1.1吗?S - 101.0?E 5.5 ?。使用通用制图工具(GMT)绘制地图和地貌模型。数据包括地形、地质、大地测量和地球物理的高分辨率网格:GEBCO、EGM2008 EGM-2008、GlobSed。结果包括模型段、坡度和截面剖面。地质作用发生在印度洋不同的演化阶段,影响着海底地貌和海沟地貌的性质。Java段具有钟形数据分布,而苏门答腊段具有双峰模式。爪哇段的重复深度最多,为-2,500至-5,200米。苏门答腊样带有两座山峰:1)一个经典的钟形山峰(- 4500米至- 5500米);2)陆架面积(0 ~ - 1750 m)。中深度(- 1750 ~ - 4500 m)的数据少于300个样本。苏门答腊岛段最常见的水深为- 4750米至- 5000米。与苏门答腊段相比,爪哇段更深。对于深度> - 6000 m,苏门答腊只有138个样本,而爪哇只有547个样本。此外,Java段具有更对称的几何形状,而苏门答腊段是不对称的,片面的。苏门答腊岛的陡度为57.86?它的东侧(面对苏门答腊岛)和14.58?在西部。Java段的陡峭度为64.34?北侧(面向爪哇岛)和24.95?在南部(面向印度洋)。本文对印度尼西亚海底地貌的研究有一定的贡献。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Java and Sumatra segments of the Sunda Trench: Geomorphology and geophysical settings analysed and visualized by GMT
The paper discusses the geomorphology of the Sunda Trench, an oceanic trench located in the eastern Indian Ocean along the Sumatra and Java Islands of the Indonesian archipelago. It analysis difference in depths and variation in slope steepness between the two segments of the trench: southern Java transect (108.8?E 10.10?S - 113.0?E 10.75?S) and northern Sumatra transect (97.5?E 1.1?S - 101.0?E 5.5?S). The maps and geomorphological modelling were plotted using Generic Mapping Tools (GMT). The data include high-resolution grids on topography, geology, geodesy and geophysics: GEBCO, EGM2008 EGM-2008, GlobSed. The results include modelled segments, slope gradients, and cross-section profiles. The geological processes take place in the Indian Ocean at different stages of its evolution and influence the nature of the submarine geomorphology and geomorphology of the trench that differs in two segments. Java segment has a bell-shaped data distribution in contrast to the Sumatra with bimodal pattern. Java segment has the most repetitive depths at -2,500 to -5,200 m. Sumatra transect has two peaks: 1) a classic bell-shaped peak (-4,500 m to -5,500 m); 2) shelf area (0 to -1,750 m). The data at middle depths (-1,750 to -4,500 m) have less than 300 samples. The most frequent bathymetry for the Sumatra segment corresponds to the -4,750 m to -5,000 m. Comparing to the Sumatra segment, the Java segment is deeper. For depths > -6,000 m, there are only 138 samples for Sumatra while 547 samples for Java. Furthermore, Java segment has a more symmetrical geometric shape while Sumatra segment is asymmetric, one-sided. The Sumatra segment has a steepness of 57.86? on its eastern side (facing Sumatra Island) and a contrasting 14.58? on the western part. The Java segment has a steepness of 64.34? on its northern side (facing Java Island) and 24.95? on the southern part (facing the Indian Ocean). The paper contributes to the studies of the submarine geomorphology in Indonesia.
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来源期刊
Glasnik - Srpskog Geografskog Drustva
Glasnik - Srpskog Geografskog Drustva Social Sciences-Education
CiteScore
0.70
自引率
0.00%
发文量
11
审稿时长
18 weeks
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