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Title: Maine Geological Survey Borehole Temperature Profiles

Abstract

This dataset includes temperature profiles from 30 boreholes throughout Maine that were selected for their depth, location, and lithologies encountered. Depths range from about 300 feet to 2,200 feet. Most of the boreholes selected for measurement were completed in granite because this lithology can be assumed to be nearly homogeneous over the depth of the borehole. Boreholes were also selected to address gaps in existing geothermal datasets. Temperature profiles were collected in October and November, 2012.

Authors:

  1. Arizona State Geological Survey
Publication Date:
Other Number(s):
265
DOE Contract Number:  
EE0002850
Research Org.:
DOE Geothermal Data Repository; Arizona State Geological Survey
Sponsoring Org.:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Program (EE-4G)
Collaborations:
Arizona State Geological Survey
Subject:
15 GEOTHERMAL ENERGY; bedrock; borehole; geospatial data; geothermal; maine; profiles; shapefile; temperature
OSTI Identifier:
1148797
DOI:
https://doi.org/10.15121/1148797

Citation Formats

Marvinney, Robert. Maine Geological Survey Borehole Temperature Profiles. United States: N. p., 2013. Web. doi:10.15121/1148797.
Marvinney, Robert. Maine Geological Survey Borehole Temperature Profiles. United States. doi:https://doi.org/10.15121/1148797
Marvinney, Robert. 2013. "Maine Geological Survey Borehole Temperature Profiles". United States. doi:https://doi.org/10.15121/1148797. https://www.osti.gov/servlets/purl/1148797. Pub date:Wed Nov 06 04:00:00 UTC 2013
@article{osti_1148797,
title = {Maine Geological Survey Borehole Temperature Profiles},
author = {Marvinney, Robert},
abstractNote = {This dataset includes temperature profiles from 30 boreholes throughout Maine that were selected for their depth, location, and lithologies encountered. Depths range from about 300 feet to 2,200 feet. Most of the boreholes selected for measurement were completed in granite because this lithology can be assumed to be nearly homogeneous over the depth of the borehole. Boreholes were also selected to address gaps in existing geothermal datasets. Temperature profiles were collected in October and November, 2012.},
doi = {10.15121/1148797},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Wed Nov 06 04:00:00 UTC 2013},
month = {Wed Nov 06 04:00:00 UTC 2013}
}