Your Twin learns with you

30% off annual Pro20% off monthly Pro

Ends in00h00m00s

Simona Pierdominici

Helmholtz Centre Potsdam – GFZ German Research Centre for Geosciences
Country flagGermany

Research Interests

Explore related searches

Articles (9)

Year:

2026

This study contributes to geothermal exploration in 1660-1520 Ma old reworked bedrock in Sweden. Our primary objectives are to constrain the orientation of horizontal stresses, and to discuss implications for geothermal exploration. High-resolution acoustic televiewer image data reveal the downhole distribution of stress indicators (borehole breakouts, drilling induced fractures and petal centerline fractures), pre-existing structures (natural fractures, foliation). About 135 m of stress indicators are measured from 0.2-1.0 km. The results suggest a uniform NNW-SSE mean maximum horizontal stress orientation. A total of 1525 pre-existing structures (natural fractures, foliation) are mapped in borehole GE-1. The prevailing stress regime controls if natural fractures and foliation are well-oriented for stimulation. For strike-slip and normal faulting stress regimes, well-oriented fractures are steeply dipping towards WSW. For a reverse faulting stress regime, shallow dipping fractures are well-oriented for simulation. The downhole distribution of stress indicators and other stress measurements in the region and other parts of Fennoscandia tentatively suggest a strike-slip stress regime, but additional studies are needed to constrain the complete stress field at study depth and towards EGS reservoir target depth. Our secondary objective is to highlight that interpretation of high-resolution acoustic data particularly in metamorphic crystalline rocks are subjective, and that more guidelines for data interpretation are needed. The interactive interpretation of the images is based on visual analyses of complex pre-existing structures and stress indicators with highly variable shapes. The application of three methods for data analyses in the GE-1 borehole propose that drilling induced fractures are little influenced by the method applied. Interpretations on individual borehole breakout azimuths may, however result in over 10 differences in orientation. Supplementary material at https://doi.org/10.6084/m9.figshare.c.7082902

Year:

2024

Year:

2024

Year:

2024

Year:

2024

Year:

2024

Year:

2024

Year:

2024

Year:

2023

Collaborators (11)

Paola Montone

Research Director

Istituto Nazionale di Geofisica e Vulcanologia

ITALY
View details

Jan-Erik Rosberg

Lund University

SWEDEN
View details

John Millett

Professor II

University of Oslo

NORWAY
View details

Luca Ziberna

University of Trieste

ITALY
View details

David Healy

University of Leeds

UNITED KINGDOM
View details

Mattia Pistone

Associate Professor

University of Georgia

UNITED STATES
View details

Donato Giovannelli

Assistant Professor

Università degli Studi di Napoli Federico II

ITALY
View details

Santanu Misra

Full Professor

Indian Institute of Technology Kanpur

View details

Silke Voigt

Goethe University Frankfurt

GERMANY
View details

Massimiliano Rinaldo BARCHI

Full Professor

University of Perugia

ITALY
View details

G Hetényi

University of Lausanne

SWITZERLAND
View details
ApplyKite TwinLearns as you apply

Make your next move.

Prepare your application

Review drafts before you send them.