Geothermal Gradient Estimation
Geothermal Gradient Estimation is a geophysical method that quantifies the rate of temperature increase with depth in the Earth's crust, distinguishing itself from other thermal assessment techniques by its reliance on in-situ temperature measurements from boreholes or wells to derive subsurface heat flow characteristics.
149
Publications
5.1K
Citations
448
Authors
187
Institutions
Publications per year
2017–2026
41
Parents
149
1–5 of 149
448
7
h-index
6
h-index
National Institute of Oceanography and Applied Geophysics, Italy
5 publications · 109 citations
5
h-index
National Research Institute of Astronomy and Geophysics, Egypt
4 publications · 133 citations
4
h-index
National Institute of Oceanography and Applied Geophysics, Italy
3 publications · 68 citations
3
h-index
1–5 of 448
187

University of Alberta
Edmonton, Canada
7 h-index
21 publications
604 citations
United States Geological Survey
Reston, United States
6 h-index
6 publications
210 citations

GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
5 h-index
6 publications
227 citations
National Institute of Oceanography and Applied Geophysics
Trieste, Italy
5 h-index
11 publications
253 citations
National Research Institute of Astronomy and Geophysics
Helwan, Egypt
4 h-index
8 publications
267 citations

Chinese Academy of Sciences
Beijing, China
4 h-index
12 publications
917 citations
Universidad Nacional Autónoma de México
Mexico City, Mexico
3 h-index
5 publications
294 citations
Geological Survey of Canada
Ottawa, Canada
3 h-index
4 publications
76 citations
1–8 of 187
JGR · 12 publications · 651 citations
11
h-index
9 publications · 192 citations
9
h-index
6 publications · 145 citations
6
h-index
5 publications · 130 citations
5
h-index
PAGEOPH · 5 publications · 102 citations
5
h-index
1–5