Advances in Earth Science at Plate Convergent Zones

A special issue of Applied Sciences (ISSN 2076-3417). This special issue belongs to the section "Earth Sciences".

Deadline for manuscript submissions: closed (20 April 2023) | Viewed by 2600

Special Issue Editors


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Guest Editor
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
Interests: tectonics; geophysics; geodynamics; geology; seismology; geochemistry;

E-Mail Website
Guest Editor
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
Interests: paleoclimate; sedimentology; source to sink relationship; evaporite
Department of Geophysics, Yunnan University, Kunming 650091, China
Interests: geophysics; geodymamics; seismicity; geomagnetics

Special Issue Information

Dear Colleagues,

Plate convergent zones are the most active tectonic settings on the Earth surface. The majority of seismicity, volcanism, and orogenesis is distributed in these regions. Various plate evolutionary processes at convergence zones have been observed and interpreted by interdisciplinary geoscientific studies, including geological, geophysical, geochemical, and geodynamic studies, which provide comprehensive insights into enigmatic plate convergent systems.

In this Special Issue, original research reviews and perspectives that describe recent advances and case studies on the Earth Sciences at the plate convergent zones are welcomed.

Dr. Yingfeng Ji
Dr. Licheng Wang
Dr. Chaodi Xie
Guest Editors

Manuscript Submission Information

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Keywords

  • geodynamics
  • geology
  • geophysics
  • geochemistry
  • plate convergent zones

Published Papers (2 papers)

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Research

10 pages, 4568 KiB  
Communication
Study TOMAS Cyclone Using Seismic Array and Single Station
by Siyin Wang, Yan Xu, Chaodi Xie and Aitang Li
Appl. Sci. 2023, 13(2), 918; https://doi.org/10.3390/app13020918 - 9 Jan 2023
Viewed by 826
Abstract
The continuous data from the YL array and four AU stations during the lifetime of the cyclone TOMAS in March 2010 were downloaded from IRIS. By performing frequency-wave number (F-K) analysis on the array data, it was found that the orientation of the [...] Read more.
The continuous data from the YL array and four AU stations during the lifetime of the cyclone TOMAS in March 2010 were downloaded from IRIS. By performing frequency-wave number (F-K) analysis on the array data, it was found that the orientation of the maximum energy of the secondary microseisms (0.1~0.5 Hz) was consistent with the movement of TOMAS when the central wind speed reached the typhoon level. The high wind speed of the cyclone could generate secondary microseisms as well as the high swell. However, the large global earthquake can affect the microseismic observations using F-K. The AU stations have a better microseism observation than the YL array, which might be due to the vibrating and tilting of the hydrophone caused by the turbulence. The F-K analysis on microseisms can produce better slowness and back azimuth observations than polarization. Full article
(This article belongs to the Special Issue Advances in Earth Science at Plate Convergent Zones)
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14 pages, 4759 KiB  
Article
Marine Geophysical Data and Its Application to Assessment of Crustal Structure along the Northern Egyptian Passive Continental Margin
by Hamdy A. M. Aboulela
Appl. Sci. 2022, 12(23), 11901; https://doi.org/10.3390/app122311901 - 22 Nov 2022
Cited by 1 | Viewed by 1049
Abstract
The Egyptian passive continental margin is considered a remarkable geologic setting, in addition to being an occupation and manufacturing locality in north Egypt. This work used accessible potential field data, such as marine gravity data, to provide a wider vision of the potential [...] Read more.
The Egyptian passive continental margin is considered a remarkable geologic setting, in addition to being an occupation and manufacturing locality in north Egypt. This work used accessible potential field data, such as marine gravity data, to provide a wider vision of the potential field of the area under investigation. The results of the two-dimensional (2D) gravity modelling revealed a good agreement between the modelled gravity and observed gravity fields, including known regional structures found in the investigated area. The findings revealed that crustal modelling was affected by the tectonic structure and the huge thickness of sedimentary layers, which act as barriers to the crystal crust. The results revealed that the crustal thickness and density are spread among the deposited layer and the inferior mantle in the Moho range. Furthermore, it was found that the basement extent lies nearly 6–9 km lower in the northern Egyptian coastline to approximately 13 km under the Herodotus abyssal plain. Moreover, it was shown that the thickness of the sedimentary layers deposit increases near the East Mediterranean Ridge. Full article
(This article belongs to the Special Issue Advances in Earth Science at Plate Convergent Zones)
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