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  1. The study is devoted to the monitoring of a geothermal reservoir by hybrid gravimetry combining different types of instruments (permanent superconducting gravimeter, absolute ballistic gravimeter, and micro-gr...

    Authors: Jacques Hinderer, Marta Calvo, Yassine Abdelfettah, Basile Hector, Umberto Riccardi, Gilbert Ferhat and Jean-Daniel Bernard
    Citation: Geothermal Energy 2015 3:16
  2. In high-enthalpy geothermal reservoirs and many other geo-technical applications, coupled non-isothermal multiphase flow is considered to be the underlying governing process that controls the system behavior. ...

    Authors: Yonghui Huang, Olaf Kolditz and Haibing Shao
    Citation: Geothermal Energy 2015 3:13
  3. The thermal regime of the Upper Rhine Graben (URG) is characterized by a series of anomalies near Soultz-sous-Forêts (France), Rittershoffen (France), and Landau (Germany). These temperature anomalies are asso...

    Authors: Jeanne Vidal, Albert Genter and Jean Schmittbuhl
    Citation: Geothermal Energy 2015 3:8
  4. The possible signature of deep fluids originating from processes occurring during infiltration or circulation in a remote valley in the Black Forest (Germany), a typical infiltration area in the crystalline ba...

    Authors: Julian Rolker, Eva Schill, Ingrid Stober, Jochen Schneider, Thomas Neumann and Thomas Kohl
    Citation: Geothermal Energy 2015 3:5
  5. The characterization of fault zones in the Bavarian Molasse Basin plays a major role for further geothermal reservoir development. Hence, their identification, geological origin, and hydraulic characterization...

    Authors: Robin Seithel, Ulrich Steiner, Birgit Müller, Christian Hecht and Thomas Kohl
    Citation: Geothermal Energy 2015 3:4
  6. Ambient noise correlation techniques are of growing interest for imaging and monitoring deep geothermal reservoirs. They are simple to implement and can be performed continuously to follow the evolution of th...

    Authors: Maximilien Lehujeur, Jérôme Vergne, Jean Schmittbuhl and Alessia Maggi
    Citation: Geothermal Energy 2015 3:3
  7. This paper reviews the state-of-the-art in hydrothermal systems in China with emphasis on current studies of potential and reservoir engineering. Three hydrothermal systems, namely, Yangbajing, Xianyang, and X...

    Authors: Yanlong Kong, Zhonghe Pang, Haibing Shao, Shengbiao Hu and Olaf Kolditz
    Citation: Geothermal Energy 2014 2:19
  8. We have made an attempt to understand the main mechanism which controls the conductive heat transfer in the Årvollskogen borehole. This has been done in order to determine the 2D subsurface temperature distrib...

    Authors: Yuriy Petrovich Maystrenko, Harald Kristian Elvebakk, Guri Venvik Ganerød, Ole Lutro, Odleiv Olesen and Jan Steinar Rønning
    Citation: Geothermal Energy 2014 2:15
  9. This study aims on investigating the regional flow field of the Soultz and adjacent geothermal fields located on the western side of the central Upper Rhine Graben and thus to provide insight into the origin o...

    Authors: Paul Baillieux, Eva Schill, Yassine Abdelfettah and Chrystel Dezayes
    Citation: Geothermal Energy 2014 2:16
  10. In reply to Geothermal Energy 2:11 comments about possible errors in our recent paper Geothermal Energy 2:6, 1-21 with title ‘Spectral analysis of aeromagnetic data for geothermal energy investigation of Ikogo...

    Authors: Ema Michael Abraham, Kolawole Muideen Lawal, Amobi Chigozie Ekwe, Owens Alile, Kehinde Ayofe Murana and Aminu Ahmed Lawal
    Citation: Geothermal Energy 2014 2:18
  11. A two-dimensional numerical model is developed for the Soultz-sous-Forêts reservoir from an idealized cross-section containing six homogeneous horizontal layers. The considered constitutive equations are those...

    Authors: Vincent Magnenet, Christophe Fond, Albert Genter and Jean Schmittbuhl
    Citation: Geothermal Energy 2014 2:17
  12. Observations in enhanced geothermal system (EGS) reservoirs of induced seismicity and slow aseismic slip ruptures on related faults suggest a close link between the two phenomena.

    Authors: Jean Schmittbuhl, Olivier Lengliné, François Cornet, Nicolas Cuenot and Albert Genter
    Citation: Geothermal Energy 2014 2:14
  13. The recent paper by Abraham et al. (2014) `Spectral analysis of aeromagnetic data for geothermal energy investigation of Ikogosi Warm Spring - Ekiti State, southwestern Nigeria’ applied spectral analysis in th...

    Authors: Levi Ikechukwu Nwankwo
    Citation: Geothermal Energy 2014 2:11
  14. The development of `enhanced geothermal systems' (EGS), designed to extract energy from deep low-enthalpy reservoirs, is opening new scenarios of growth for the whole geothermal sector. A relevant tool to esti...

    Authors: Martino Lacirignola, Bechara Hage Meany, Pierryves Padey and Isabelle Blanc
    Citation: Geothermal Energy 2014 2:8
  15. Geothermal systems are commonly hosted in highly altered and fractured rock. As a result, the relationships between physical properties such as strength and permeability can be complex. Understanding such prop...

    Authors: Paul A Siratovich, Michael J Heap, Marlène C Villenueve, James W Cole and Thierry Reuschlé
    Citation: Geothermal Energy 2014 2:10
  16. Aeromagnetic data of the Ikogosi warm spring region was used to calculate the basal depth of the magnetic layer (Curie point depth) in the region. The warm spring issues from a crossing of fractures from a met...

    Authors: Ema Michael Abraham, Kolawole Muideen Lawal, Amobi Chigozie Ekwe, Owens Alile, Kehinde Ayofe Murana and Aminu Ahmed Lawal
    Citation: Geothermal Energy 2014 2:6
  17. The thermal springs of Rajapur situated along the west coast of Maharashtra and parts of high-heat-generating granites of Gugi in Karnataka (India) seem to be genetically related. The present investigation inv...

    Authors: Hemant K Singh, Yadvendra Kumar, Dornadula Chandrasekharam, Trupti Gurav and Banambar Singh
    Citation: Geothermal Energy 2014 2:2
  18. We present three-dimensional simulation of cooling of 63 models of a magma chamber in the Los Azufres geothermal field by varying the top of the chamber depth between 5 and 9 km (centroid from about 7 to 13 km...

    Authors: Surendra P Verma and Efraín Gómez-Arias
    Citation: Geothermal Energy 2013 1:5

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