Trần Thanh Tuấn, Phó giáo sư, Tiến sĩ
Chức vụ Bộ môn:
Phó Trưởng Bộ môn
Văn phòng:
T3-306
Thư điện tử VNU:
tuantt
Trang web:
user.hus.edu.vn/tranthanhtuan
Lĩnh vực nghiên cứu:
Sóng trong môi trường đàn hồi, Kỹ thuật tỷ số H/V
Quá trình đào tạo:
- 2006-2009: Đại học Friedrich-Schiller-University Jena, Germany, Tiến sỹ Địa chấn tại General Geophysics Department, Institute of Geosciences.
- 2002-2004: Đại học KHTN, Vietnam, Thạc sỹ Cơ học.
- 1998-2002: Chương trình Cử nhân tài năng, Hanoi University of Sciences, Vietnam, Cử nhân Toán Cơ.
Các môn giảng dạy:
- Cơ học lý thuyết
- Phép tính Tensor
- Đại số tuyến tính
- Giải tích
Hoạt động khoa học:
- 03/2010-07/2010: Short Visiting Scholar, Math department, University of Washington, Seattle, USA
- 01/2014-12/2019: Junior Associate at ICTP, Trieste, Italy
- 01/2020-12/2015: Regular Asscociate at ICTP, Trieste, Italy
Công bố khoa học
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. Reflection and transmission of SH waves at a very rough interface and its band gaps. Journal of Sound and Vibration. 2017;411:422–434.
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. Approximate formula for the H/V ratio of Rayleigh waves in incompressible orthotropic half-spaces coated by a thin elastic layer. Vietnam Journal of Mechanics. 2017;39:365–374.
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. Reflection and transmission of SH waves at a very rough interface and its band gaps. Journal of Sound and Vibration. 2017;411:422–434.
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. An Improved Formula of Fundamental Resonance Frequency of a Layered Half-Space Model Used in H/V Ratio Technique. Pure and Applied Geophysics. 2016:1–10.
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. The dispersion of Rayleigh waves in orthotropic layered half-space using matrix method. Vietnam Journal of Mechanics. 2016;38:27–38.
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. An improved formula of fundamental resonance frequency of a layered half-space model used in H/V ratio technique. Pure and Applied Geophysics. 2016;173:2803–2812.
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. Approximate formula of peak frequency of H/V ratio curve in multilayered model and its use in H/V ratio technique. Pure and Applied Geophysics. 2015;173(2):487–498.
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. On the relationship of peaks and troughs of the ellipticity (H/V) of Rayleigh waves and the transmission response of single layer over half-space models. Geophysical Journal International. 2011;184:793–800.


