Eruption frequency and magnitude in a geothermally active continental rift: The Bora-Baricha-Tulla Moye volcanic complex, Main Ethiopian Rift

Publikationen: Beitrag in FachzeitschriftArtikelForschung(peer-reviewed)

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Eruption frequency and magnitude in a geothermally active continental rift: The Bora-Baricha-Tulla Moye volcanic complex, Main Ethiopian Rift. / Tadesse, Amdemichael Zafu; Fontijn, Karen; Melaku, Abate A. et al.
in: Journal of volcanology and geothermal research, Jahrgang 423.2022, Nr. March, 15.01.2022, S. 629-667.

Publikationen: Beitrag in FachzeitschriftArtikelForschung(peer-reviewed)

Harvard

Tadesse, AZ, Fontijn, K, Melaku, AA, Gebru, Smith, V, Tomlinson, EL, Barford, DN, Gopon, P, Bégué, F, Caricchi, L, Laha, P, Terryn, HA, Gudbrandsson, S, Yirgu, G & Ayalew, D 2022, 'Eruption frequency and magnitude in a geothermally active continental rift: The Bora-Baricha-Tulla Moye volcanic complex, Main Ethiopian Rift', Journal of volcanology and geothermal research, Jg. 423.2022, Nr. March, S. 629-667. https://doi.org/10.1016/j.jvolgeores.2022.107471

APA

Tadesse, A. Z., Fontijn, K., Melaku, A. A., Gebru, Smith, V., Tomlinson, E. L., Barford, D. N., Gopon, P., Bégué, F., Caricchi, L., Laha, P., Terryn, H. A., Gudbrandsson, S., Yirgu, G., & Ayalew, D. (2022). Eruption frequency and magnitude in a geothermally active continental rift: The Bora-Baricha-Tulla Moye volcanic complex, Main Ethiopian Rift. Journal of volcanology and geothermal research, 423.2022(March), 629-667. https://doi.org/10.1016/j.jvolgeores.2022.107471

Vancouver

Tadesse AZ, Fontijn K, Melaku AA, Gebru, Smith V, Tomlinson EL et al. Eruption frequency and magnitude in a geothermally active continental rift: The Bora-Baricha-Tulla Moye volcanic complex, Main Ethiopian Rift. Journal of volcanology and geothermal research. 2022 Jan 15;423.2022(March):629-667. doi: 10.1016/j.jvolgeores.2022.107471

Author

Tadesse, Amdemichael Zafu ; Fontijn, Karen ; Melaku, Abate A. et al. / Eruption frequency and magnitude in a geothermally active continental rift : The Bora-Baricha-Tulla Moye volcanic complex, Main Ethiopian Rift. in: Journal of volcanology and geothermal research. 2022 ; Jahrgang 423.2022, Nr. March. S. 629-667.

Bibtex - Download

@article{fb91fd4972f145beb0754f5889f6f0fd,
title = "Eruption frequency and magnitude in a geothermally active continental rift: The Bora-Baricha-Tulla Moye volcanic complex, Main Ethiopian Rift",
abstract = "Based on the review of a wide range of literature, this paper finds that: (1) the average specific surface energy of various single crystals is only 0.8 J/m2. (2) The average specific fracture energy of the rocks with a pre-crack under static cleavage tests is 4.6 J/m2. (3) The average specific fracture energy of the rocks with a pre-cut notch but with no pre-crack under static tensile fracture (mode I) tests is 4.6 J/m2. (4) The average specific fracture energies of regular rock specimens with neither pre-made crack nor pre-cut notch are 26.6, 13.9 and 25.7 J/m2 under uniaxial compression, tension and shear tests, respectively. (5) The average specific fracture energy of irregular single quartz particles under uniaxial compression is 13.8 J/m2. (6) The average specific fracture energy of particle beds under drop weight tests is 74.0 J/m2. (7) The average specific fracture energy of multi-particles in milling tests is 72.5 J/m2. (8) The average specific energy of rocks in percussive drilling is 399 J/m3, that in full-scale cutting is 131 J/m3, and that in rotary drilling is 157 J/m3. (9) The average energy efficiency of milling is only 1.10%. (10) The accurate measurements of specific fracture energy in blasting are too few to draw reliable conclusions. In the last part of the paper, the effects of inter-granular displacement, loading rate, confining pressure, surface area measurement, premade crack, attrition and thermal energy on the specific fracture energy of rock are discussed.",
author = "Tadesse, {Amdemichael Zafu} and Karen Fontijn and Melaku, {Abate A.} and Gebru and Victoria Smith and Tomlinson, {Emma L.} and Barford, {Dan N.} and Phillip Gopon and Florence B{\'e}gu{\'e} and Luca Caricchi and Priya Laha and Terryn, {Herman A.} and Snorri Gudbrandsson and Gezahegn Yirgu and Dereje Ayalew",
year = "2022",
month = jan,
day = "15",
doi = "10.1016/j.jvolgeores.2022.107471",
language = "English",
volume = "423.2022",
pages = "629--667",
journal = "Journal of volcanology and geothermal research",
issn = "0377-0273",
publisher = "Elsevier B.V.",
number = "March",

}

RIS (suitable for import to EndNote) - Download

TY - JOUR

T1 - Eruption frequency and magnitude in a geothermally active continental rift

T2 - The Bora-Baricha-Tulla Moye volcanic complex, Main Ethiopian Rift

AU - Tadesse, Amdemichael Zafu

AU - Fontijn, Karen

AU - Melaku, Abate A.

AU - Gebru, null

AU - Smith, Victoria

AU - Tomlinson, Emma L.

AU - Barford, Dan N.

AU - Gopon, Phillip

AU - Bégué, Florence

AU - Caricchi, Luca

AU - Laha, Priya

AU - Terryn, Herman A.

AU - Gudbrandsson, Snorri

AU - Yirgu, Gezahegn

AU - Ayalew, Dereje

PY - 2022/1/15

Y1 - 2022/1/15

N2 - Based on the review of a wide range of literature, this paper finds that: (1) the average specific surface energy of various single crystals is only 0.8 J/m2. (2) The average specific fracture energy of the rocks with a pre-crack under static cleavage tests is 4.6 J/m2. (3) The average specific fracture energy of the rocks with a pre-cut notch but with no pre-crack under static tensile fracture (mode I) tests is 4.6 J/m2. (4) The average specific fracture energies of regular rock specimens with neither pre-made crack nor pre-cut notch are 26.6, 13.9 and 25.7 J/m2 under uniaxial compression, tension and shear tests, respectively. (5) The average specific fracture energy of irregular single quartz particles under uniaxial compression is 13.8 J/m2. (6) The average specific fracture energy of particle beds under drop weight tests is 74.0 J/m2. (7) The average specific fracture energy of multi-particles in milling tests is 72.5 J/m2. (8) The average specific energy of rocks in percussive drilling is 399 J/m3, that in full-scale cutting is 131 J/m3, and that in rotary drilling is 157 J/m3. (9) The average energy efficiency of milling is only 1.10%. (10) The accurate measurements of specific fracture energy in blasting are too few to draw reliable conclusions. In the last part of the paper, the effects of inter-granular displacement, loading rate, confining pressure, surface area measurement, premade crack, attrition and thermal energy on the specific fracture energy of rock are discussed.

AB - Based on the review of a wide range of literature, this paper finds that: (1) the average specific surface energy of various single crystals is only 0.8 J/m2. (2) The average specific fracture energy of the rocks with a pre-crack under static cleavage tests is 4.6 J/m2. (3) The average specific fracture energy of the rocks with a pre-cut notch but with no pre-crack under static tensile fracture (mode I) tests is 4.6 J/m2. (4) The average specific fracture energies of regular rock specimens with neither pre-made crack nor pre-cut notch are 26.6, 13.9 and 25.7 J/m2 under uniaxial compression, tension and shear tests, respectively. (5) The average specific fracture energy of irregular single quartz particles under uniaxial compression is 13.8 J/m2. (6) The average specific fracture energy of particle beds under drop weight tests is 74.0 J/m2. (7) The average specific fracture energy of multi-particles in milling tests is 72.5 J/m2. (8) The average specific energy of rocks in percussive drilling is 399 J/m3, that in full-scale cutting is 131 J/m3, and that in rotary drilling is 157 J/m3. (9) The average energy efficiency of milling is only 1.10%. (10) The accurate measurements of specific fracture energy in blasting are too few to draw reliable conclusions. In the last part of the paper, the effects of inter-granular displacement, loading rate, confining pressure, surface area measurement, premade crack, attrition and thermal energy on the specific fracture energy of rock are discussed.

U2 - 10.1016/j.jvolgeores.2022.107471

DO - 10.1016/j.jvolgeores.2022.107471

M3 - Article

VL - 423.2022

SP - 629

EP - 667

JO - Journal of volcanology and geothermal research

JF - Journal of volcanology and geothermal research

SN - 0377-0273

IS - March

ER -