Abstract
A preliminary heat flow map of Europe was prepared, based on data contained in 401 references. The map was prepared on a scale of 1:5,000,000 and shows broad-scale geological structure (e.g., platforms, shields, foredeeps) and specialized rock suites (ophiolites, volcanites). Primary faults and thrust faults are indicated, and contours showing the depth of crystalline basement are given. Heat flow is plotted using 10.0 mW/m/sup 2/ isotherms. The accompanying explanatory text describes data acquisition and techniques of correction, and discusses some implications of the results.
Citation Formats
Cermak, V., and Hurtig, E.
Preliminary heat flow map of Europe. Explanatory text.
Germany: N. p.,
1977.
Web.
Cermak, V., & Hurtig, E.
Preliminary heat flow map of Europe. Explanatory text.
Germany.
Cermak, V., and Hurtig, E.
1977.
"Preliminary heat flow map of Europe. Explanatory text."
Germany.
@misc{etde_5218361,
title = {Preliminary heat flow map of Europe. Explanatory text}
author = {Cermak, V., and Hurtig, E.}
abstractNote = {A preliminary heat flow map of Europe was prepared, based on data contained in 401 references. The map was prepared on a scale of 1:5,000,000 and shows broad-scale geological structure (e.g., platforms, shields, foredeeps) and specialized rock suites (ophiolites, volcanites). Primary faults and thrust faults are indicated, and contours showing the depth of crystalline basement are given. Heat flow is plotted using 10.0 mW/m/sup 2/ isotherms. The accompanying explanatory text describes data acquisition and techniques of correction, and discusses some implications of the results.}
place = {Germany}
year = {1977}
month = {Aug}
}
title = {Preliminary heat flow map of Europe. Explanatory text}
author = {Cermak, V., and Hurtig, E.}
abstractNote = {A preliminary heat flow map of Europe was prepared, based on data contained in 401 references. The map was prepared on a scale of 1:5,000,000 and shows broad-scale geological structure (e.g., platforms, shields, foredeeps) and specialized rock suites (ophiolites, volcanites). Primary faults and thrust faults are indicated, and contours showing the depth of crystalline basement are given. Heat flow is plotted using 10.0 mW/m/sup 2/ isotherms. The accompanying explanatory text describes data acquisition and techniques of correction, and discusses some implications of the results.}
place = {Germany}
year = {1977}
month = {Aug}
}