Chandrasekaram, D.

Profile URL
https://hdl.handle.net/11147/16593
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Main Affiliation
03.09. Department of Materials Science and Engineering
Status
Current Staff
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Scopus Author ID
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WoS Researcher ID

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Scholarly Output

2

Articles

1

Views / Downloads

813/21

Supervised MSc Theses

0

Supervised PhD Theses

0

WoS Citation Count

0

Scopus Citation Count

1

Patents

0

Projects

0

WoS Citations per Publication

0.00

Scopus Citations per Publication

0.50

Open Access Source

0

Supervised Theses

0

JournalCount
Geothermal Systems and Energy Resources: Turkey and Greece1
Journal of Earth System Science1
Current Page: 1 / 1

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Author of Publication: search.filters.isAuthorOfPublication.b135ebfb-89c8-42b6-b835-0f2477dc221f

Scholarly Output Search Results

Now showing 1 - 2 of 2
  • Book Part
    Geothermal Systems and Energy Resources Turkey and Greece Foreword
    (Taylor and Francis Ltd., 2014) Baba, Alper; Baba, Alper; Bundschuh, Jochen; Chandrasekaram, D.; Chandrasekaram, D.; 03.09. Department of Materials Science and Engineering; 03.03. Department of Civil Engineering; 03. Faculty of Engineering; 01. Izmir Institute of Technology
    [No abstract available]
  • Article
    Citation - Scopus: 1
    Audio-magnetotelluric (amt) studies over rajapur hot spring in west coast maharashtra, India
    (indian Acad Sciences, 2024) Deshmukh, Vasu; Chandrasekaram, D.; Kumar, P. V. Vijaya; Chandrasekaram, D.; Raju, Khasi; Sathishkumar, S.; Srinivas, Y.; Rao, P. B. V. Subba; 03.09. Department of Materials Science and Engineering; 03. Faculty of Engineering; 01. Izmir Institute of Technology
    In the west coast geothermal provinces, the Rajapur hot spring, located in the southern part of western Maharashtra, is well thought to originate from the interaction of meteoric water with the granitic basement. A 3D AMT survey was conducted to determine the geo-electrical structure of the hot spring. Dimensionality analysis carried out by phase tensor analysis reveals complex subsurface 3D structures. 2D and 3D modelling have yielded three distinct resistivity layers in the Rajapur geothermal field. These layers include a moderately resistive surface layer representing weathered Deccan traps having a thickness of about 100 m, a conductive second layer with a thickness of about 100-400 m represents Kaladgi sediments and a deeper high resistive layer (0.5-1.0 km) representing granitic gneisses basement. High conductivity anomaly within the Kaladgi sediments represents a hydrothermal reservoir that is associated with faults/fractures beneath the Deccan Traps.