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Cape EGS: Seismic Attenuation Profile and DAS Microseismic P-wave Spectra

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This dataset contains a 1D P-wave attenuation (Q) profile, distributed acoustic sensing (DAS) microseismic P-wave spectra, and derived source parameters from the Delano 1OB well at the Cape Modern geothermal field. The data were collected during a stimulation period from mid-February to mid-March 2024 and include approximately 6,700 microseismic events. Frequency-independent Q values for the upper ~2.5 km are estimated using along-depth spectral ratios in the 20-200 Hz band, based on overlapping channel stacks. The dataset also includes well log measurements (e.g., density, P-wave velocity, and derived shear modulus) summarized using median and median absolute deviation statistics at each channel depth.

Microseismic source parameters are derived using a single-spectral fitting approach based on the Brune model, with event-level results reported as median values across selected channels that meet quality control criteria. The dataset further provides raw DAS P-wave arrival spectra calculated over 0.1 s windows, associated noise spectra, event origin times, and DAS channel configuration information, including spatial coordinates and depth conversion parameters. Python scripts are included to read, process, and visualize the data products. The methods used to compute attenuation and source parameters are described in Chang et al. (submitted), which will be linked upon publication: Chang, H., Nakata, N., Abercrombie, R. E., Dadi, S. & Titov, T. (submitted). Characterizing shallow attenuation and microearthquake source parameters using a downhole DAS array at the Cape Modern geothermal field.

Citation Formats

TY - DATA AB - This dataset contains a 1D P-wave attenuation (Q) profile, distributed acoustic sensing (DAS) microseismic P-wave spectra, and derived source parameters from the Delano 1OB well at the Cape Modern geothermal field. The data were collected during a stimulation period from mid-February to mid-March 2024 and include approximately 6,700 microseismic events. Frequency-independent Q values for the upper ~2.5 km are estimated using along-depth spectral ratios in the 20-200 Hz band, based on overlapping channel stacks. The dataset also includes well log measurements (e.g., density, P-wave velocity, and derived shear modulus) summarized using median and median absolute deviation statistics at each channel depth. Microseismic source parameters are derived using a single-spectral fitting approach based on the Brune model, with event-level results reported as median values across selected channels that meet quality control criteria. The dataset further provides raw DAS P-wave arrival spectra calculated over 0.1 s windows, associated noise spectra, event origin times, and DAS channel configuration information, including spatial coordinates and depth conversion parameters. Python scripts are included to read, process, and visualize the data products. The methods used to compute attenuation and source parameters are described in Chang et al. (submitted), which will be linked upon publication: Chang, H., Nakata, N., Abercrombie, R. E., Dadi, S. & Titov, T. (submitted). Characterizing shallow attenuation and microearthquake source parameters using a downhole DAS array at the Cape Modern geothermal field. AU - Chang, Hilary A2 - Nakata, Nori A3 - Abercrombie, Rachel A4 - Dadi, Sireesh A5 - Titov, Aleksei DB - Open Energy Data Initiative (OEDI) DP - Open EI | National Laboratory of the Rockies DO - KW - geothermal KW - energy KW - DAS KW - fiber-optic KW - attenuation KW - microseismicity KW - P-wave KW - source parameters KW - stress drop KW - cape KW - forge KW - Q KW - spectra KW - seismic KW - EGS KW - Cape Modern KW - Utah FORGE KW - distributed acoustic sensing KW - P-wave attenuation KW - quality factor KW - Brune model KW - corner frequency KW - seismic moment KW - moment magnitude KW - well logs KW - downhole measurements KW - raw data KW - processed data KW - geomechanics KW - geophysics LA - English DA - 2026/03/17 PY - 2026 PB - Lamont Doherty Earth Observatory T1 - Cape EGS: Seismic Attenuation Profile and DAS Microseismic P-wave Spectra UR - https://data.openei.org/submissions/8664 ER -
Export Citation to RIS
Chang, Hilary, et al. Cape EGS: Seismic Attenuation Profile and DAS Microseismic P-wave Spectra. Lamont Doherty Earth Observatory, 17 March, 2026, GDR. https://gdr.openei.org/submissions/1823.
Chang, H., Nakata, N., Abercrombie, R., Dadi, S., & Titov, A. (2026). Cape EGS: Seismic Attenuation Profile and DAS Microseismic P-wave Spectra. [Data set]. GDR. Lamont Doherty Earth Observatory. https://gdr.openei.org/submissions/1823
Chang, Hilary, Nori Nakata, Rachel Abercrombie, Sireesh Dadi, and Aleksei Titov. Cape EGS: Seismic Attenuation Profile and DAS Microseismic P-wave Spectra. Lamont Doherty Earth Observatory, March, 17, 2026. Distributed by GDR. https://gdr.openei.org/submissions/1823
@misc{OEDI_Dataset_8664, title = {Cape EGS: Seismic Attenuation Profile and DAS Microseismic P-wave Spectra}, author = {Chang, Hilary and Nakata, Nori and Abercrombie, Rachel and Dadi, Sireesh and Titov, Aleksei}, abstractNote = {This dataset contains a 1D P-wave attenuation (Q) profile, distributed acoustic sensing (DAS) microseismic P-wave spectra, and derived source parameters from the Delano 1OB well at the Cape Modern geothermal field. The data were collected during a stimulation period from mid-February to mid-March 2024 and include approximately 6,700 microseismic events. Frequency-independent Q values for the upper ~2.5 km are estimated using along-depth spectral ratios in the 20-200 Hz band, based on overlapping channel stacks. The dataset also includes well log measurements (e.g., density, P-wave velocity, and derived shear modulus) summarized using median and median absolute deviation statistics at each channel depth.

Microseismic source parameters are derived using a single-spectral fitting approach based on the Brune model, with event-level results reported as median values across selected channels that meet quality control criteria. The dataset further provides raw DAS P-wave arrival spectra calculated over 0.1 s windows, associated noise spectra, event origin times, and DAS channel configuration information, including spatial coordinates and depth conversion parameters. Python scripts are included to read, process, and visualize the data products. The methods used to compute attenuation and source parameters are described in Chang et al. (submitted), which will be linked upon publication: Chang, H., Nakata, N., Abercrombie, R. E., Dadi, S. \& Titov, T. (submitted). Characterizing shallow attenuation and microearthquake source parameters using a downhole DAS array at the Cape Modern geothermal field.}, url = {https://gdr.openei.org/submissions/1823}, year = {2026}, howpublished = {GDR, Lamont Doherty Earth Observatory, https://gdr.openei.org/submissions/1823}, note = {Accessed: 2026-05-17} }

Details

Data from Mar 17, 2026

Last updated Apr 20, 2026

Submitted Mar 17, 2026

Organization

Lamont Doherty Earth Observatory

Contact

Hilary Chang

Authors

Hilary Chang

Lamont-Doherty Earth Observatory

Nori Nakata

Lawrence Berkeley National Laboratory

Rachel Abercrombie

Boston University

Sireesh Dadi

Fervo Energy

Aleksei Titov

Fervo Energy

Research Areas

DOE Project Details

Project Name Collection of Microearthquake Data for Mitigating, Characterizing, and Understanding Induced Seismicity for Optimizing the Performance of EGS (MEQ)

Project Lead Zachary Frone

Project Number 26525

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