Palaeoclimatic temperature signals — can they be washed out?
- 15 June 1998
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 291 (1-4) , 225-234
- https://doi.org/10.1016/s0040-1951(98)00042-0
Abstract
No abstract availableThis publication has 12 references indexed in Scilit:
- The thermal regime of the crystalline continental crust: Implications from the KTBJournal of Geophysical Research, 1997
- Palaeoclimate and structure: the most important factors controlling subsurface temperatures in crystalline rocks. A case history from Outokumpu, eastern FinlandGeophysical Journal International, 1996
- Thermal and hydraulic aspects of the KTB drill siteGeophysical Journal International, 1996
- Deriving century‐long trends of surface temperature change from borehole temperaturesGeophysical Research Letters, 1996
- Coupled hydraulic, thermal and mechanical considerations for the simulation of hot dry rock reservoirsGeothermics, 1995
- Heat advection versus conduction at the KTB: possible reasons for vertical variations in heat-flow densityGeophysical Journal International, 1994
- An attempt to interpret the temperature profile of the KTB pilot drillhole (Germany) by paleoclimatic considerationsPalaeogeography, Palaeoclimatology, Palaeoecology, 1992
- Least squares inversion of borehole temperature measurements in functional spaceJournal of Geophysical Research, 1991
- On the thermal effects of groundwater flow: 1. Regional scale systemsJournal of Geophysical Research, 1983
- Geotherms of Lake Superior Copper CountryGSA Bulletin, 1923