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Tìm kiếm theo: Tác giả Vu, Van Tich

Duyệt theo: 0-9 A B C D E F G H I J K L M N O P Q R S T U V W X Y Z
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  • Geothermal Renewable Energy in Vietnam: A Current Status Overview and Proposing Solutions for Development

    • Tác giả : Hoang, Van Hiep; Vu, Van Tich; Tran, Trong Thang; Pham, Xuan Anh; Phan, Thanh Tung (2019)

  • Climate change and energy are two of the biggest challenges in the world and Vietnam today. To resolve the mentioned above problem, especially the energy shortage, studying renewable energy systems is becoming necessary. This paper investigates the current status of renewable geothermal energy in Vietnam. This study focuses on determining the heat source based on geo thermometric calculations of K+ - Na+ cations from thermal water in the most 18 potential geothermal sources (in the northern part of Vietnam) in combination with the assessment of groundwater potential by the hydrogeological survey. With the deep temperatures of reservoirs are varied from 136oC to 170oC, these geothermal...
  • Tectonophysics Volume 393 issue 1-4 2004 [doi 10.1016%2Fj.tecto.2004.07.030] C. Lepvrier; H. Maluski; Vu Van Tich; A. Leyreloup; Phan Truong -- The Early Triassic Indosinian orogeny in Vietnam (Truong.pdf.jpg
  • Article

  • The Early Triassic Indosinian orogeny in Vietnam (Truong Son Belt and Kontum Massif); implications for the geodynamic evolution of Indochina

    • Tác giả : Lepvrier, C.; Maluski, H.; Vu, Van Tich; Leyreloup, A.; Phan, Truong Thi; Nguyen, Van Vuong (2004)

  • New structural field data at various scale and 40Ar–39Ar geochronological results, from the basement rocks in the Truong Son belt and Kontum Massif of Vietnam, confirm that ductile deformation and high-temperature metamorphism were caused by the Early Triassic event of the Indosinian Orogeny in the range of 250–240 Ma. A compilation of isotopic data obtained in other countries along the Sibumasu–Indochina boundary broadly indicates same interval of ages. This tectonothermal event is interpreted as the result of a synchronous oblique collision of Indochina with both Sibumasu and South China, inducing dextral and sinistral shearing along E–W to NW–SE and N–S fault zones, respectively. T...

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Tìm kiếm theo: Tác giả Vu, Van Tich

Duyệt theo: 0-9 A B C D E F G H I J K L M N O P Q R S T U V W X Y Z
Hoặc nhập chữ cái đầu tiên:  
Kết quả tìm kiếm từ 1 đến 3 trong 3 kết quả
  • item.jpg
  • Conference Paper

  • Geothermal Renewable Energy in Vietnam: A Current Status Overview and Proposing Solutions for Development

    • Tác giả : Hoang, Van Hiep; Vu, Van Tich; Tran, Trong Thang; Pham, Xuan Anh; Phan, Thanh Tung (2019)

  • Climate change and energy are two of the biggest challenges in the world and Vietnam today. To resolve the mentioned above problem, especially the energy shortage, studying renewable energy systems is becoming necessary. This paper investigates the current status of renewable geothermal energy in Vietnam. This study focuses on determining the heat source based on geo thermometric calculations of K+ - Na+ cations from thermal water in the most 18 potential geothermal sources (in the northern part of Vietnam) in combination with the assessment of groundwater potential by the hydrogeological survey. With the deep temperatures of reservoirs are varied from 136oC to 170oC, these geothermal...
  • Tectonophysics Volume 393 issue 1-4 2004 [doi 10.1016%2Fj.tecto.2004.07.030] C. Lepvrier; H. Maluski; Vu Van Tich; A. Leyreloup; Phan Truong -- The Early Triassic Indosinian orogeny in Vietnam (Truong.pdf.jpg
  • Article

  • The Early Triassic Indosinian orogeny in Vietnam (Truong Son Belt and Kontum Massif); implications for the geodynamic evolution of Indochina

    • Tác giả : Lepvrier, C.; Maluski, H.; Vu, Van Tich; Leyreloup, A.; Phan, Truong Thi; Nguyen, Van Vuong (2004)

  • New structural field data at various scale and 40Ar–39Ar geochronological results, from the basement rocks in the Truong Son belt and Kontum Massif of Vietnam, confirm that ductile deformation and high-temperature metamorphism were caused by the Early Triassic event of the Indosinian Orogeny in the range of 250–240 Ma. A compilation of isotopic data obtained in other countries along the Sibumasu–Indochina boundary broadly indicates same interval of ages. This tectonothermal event is interpreted as the result of a synchronous oblique collision of Indochina with both Sibumasu and South China, inducing dextral and sinistral shearing along E–W to NW–SE and N–S fault zones, respectively. T...