Subsurface structural control of geothermal resources in a magmatic rift: gravity and magnetic study of the Tulu Moye geothermal prospect, Main Ethiopian Rift
Subsurface structural control of geothermal resources in a magmatic rift: gravity and magnetic study of the Tulu Moye geothermal prospect, Main Ethiopian Rift
Since the Quaternary, extension and magmatism in the Main Ethiopian Rift (MER) have been mainly focused into narrow magmatic segments that have numerous volcanic centers and caldera collapses that offer favorable conditions for the occurrence of geothermal resources. However, the subsurface structure of the volcanic systems (0–10 km) and their link to the distribution of shallow geothermal resources remain unclear. To investigate the role of subsurface structures on the occurrence of these resources, we conducted gravity and magnetic studies combined with geological constraints within the Tulu Moye Geothermal Prospect (TMGP), one of the current geothermal prospects in the central MER associated with caldera collapses. Gravity data from the Global Gravity Model plus (GGMplus 2013) and ground magnetic data transformed into residual and derivative maps reveal that shallow magmatic intrusions occur under the volcanic centers (Tulu Moye, Bora, and Bericha). Our interpretation along with recent magnetotelluric model suggests that only the intrusion beneath Tulu Moye is currently magmatically active and includes partial melt, consistent with it being a primary heat source for the geothermal system. A new caldera formation model is proposed where the TMGP hosts an older large caldera (about 25 km diameter) within which there are several smaller nested caldera systems associated with the Bora, Bericha, and Tulu Moye volcanoes. Along with existing geologic, seismic, and magnetotelluric studies, our gravity and magnetic analysis indicate the interaction between NNE-SSW (rift-parallel) and NW-SE (cross-rift) trending faults, along with shallow magmatic intrusions and caldera systems, suggesting that such a large geothermal system is possible under these conditions.
Nigussie, Wubamlak
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Alemu, Abera
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Mickus, Kevin
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Keir, Derek
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Demissie, Zelalem
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Muhabaw, Yoseph
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Muluneh, Ameha
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Corti, Giacomo
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Yehualaw, Esubalew
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1 October 2023
Nigussie, Wubamlak
69c11fa3-ad0f-4a84-adef-e9f5efce3d78
Alemu, Abera
e97a8b62-f02b-499c-aedd-4c00a34694e1
Mickus, Kevin
1d2af94a-3c62-42be-8e34-c438f112cd32
Keir, Derek
5616f81f-bf1b-4678-a167-3160b5647c65
Demissie, Zelalem
d9ae17ed-2aa6-4d9b-a1cb-73154142f893
Muhabaw, Yoseph
cbe75ff0-6bec-4d9a-be90-55c3cd1754ac
Muluneh, Ameha
9c48408f-650f-49ad-9133-bc201fa817ce
Corti, Giacomo
dce88b12-5b7a-43b1-8a58-5bd1bc13634c
Yehualaw, Esubalew
e332fde1-b1bb-4ea2-8428-6b48c8d9e19c
Nigussie, Wubamlak, Alemu, Abera, Mickus, Kevin, Keir, Derek, Demissie, Zelalem, Muhabaw, Yoseph, Muluneh, Ameha, Corti, Giacomo and Yehualaw, Esubalew
(2023)
Subsurface structural control of geothermal resources in a magmatic rift: gravity and magnetic study of the Tulu Moye geothermal prospect, Main Ethiopian Rift.
Frontiers in Earth Science, 11, [1181533].
(doi:10.3389/feart.2023.1181533).
Abstract
Since the Quaternary, extension and magmatism in the Main Ethiopian Rift (MER) have been mainly focused into narrow magmatic segments that have numerous volcanic centers and caldera collapses that offer favorable conditions for the occurrence of geothermal resources. However, the subsurface structure of the volcanic systems (0–10 km) and their link to the distribution of shallow geothermal resources remain unclear. To investigate the role of subsurface structures on the occurrence of these resources, we conducted gravity and magnetic studies combined with geological constraints within the Tulu Moye Geothermal Prospect (TMGP), one of the current geothermal prospects in the central MER associated with caldera collapses. Gravity data from the Global Gravity Model plus (GGMplus 2013) and ground magnetic data transformed into residual and derivative maps reveal that shallow magmatic intrusions occur under the volcanic centers (Tulu Moye, Bora, and Bericha). Our interpretation along with recent magnetotelluric model suggests that only the intrusion beneath Tulu Moye is currently magmatically active and includes partial melt, consistent with it being a primary heat source for the geothermal system. A new caldera formation model is proposed where the TMGP hosts an older large caldera (about 25 km diameter) within which there are several smaller nested caldera systems associated with the Bora, Bericha, and Tulu Moye volcanoes. Along with existing geologic, seismic, and magnetotelluric studies, our gravity and magnetic analysis indicate the interaction between NNE-SSW (rift-parallel) and NW-SE (cross-rift) trending faults, along with shallow magmatic intrusions and caldera systems, suggesting that such a large geothermal system is possible under these conditions.
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feart-11-1181533
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Accepted/In Press date: 13 July 2023
e-pub ahead of print date: 26 July 2023
Published date: 1 October 2023
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Local EPrints ID: 486918
URI: http://eprints.soton.ac.uk/id/eprint/486918
PURE UUID: 262e2898-7d81-4e0f-be59-a34c8e6d9463
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Date deposited: 08 Feb 2024 17:40
Last modified: 18 Mar 2024 03:18
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Author:
Wubamlak Nigussie
Author:
Abera Alemu
Author:
Kevin Mickus
Author:
Zelalem Demissie
Author:
Yoseph Muhabaw
Author:
Ameha Muluneh
Author:
Giacomo Corti
Author:
Esubalew Yehualaw
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