Welkom op het expertplatform!
Dit platform verschaft informatie en kennis omtrent de WL expertisedomeinen 'hydraulica en sediment', 'havens en waterwegen', 'waterbouwkundige constructies', 'waterbeheer' en 'kustbescherming' - gaande van WL medewerkers met hun expertise, het curriculum van deze instelling, tot publicaties, projecten, data (op termijn) en evenementen waarin het WL betrokken is.
Het WL onderschrijft het belang van "open access" voor de ontsluiting van haar onderzoeksresultaten. Lees er meer over in ons openaccessbeleid.
Lake Issyk-Kul (Tien Shan): Unusually low heat flow in an active intermontane basin
Vermeesch, P.; Poort, J.; Duchkov, A. D. ; Klerkx, J.; De Batist, M. (2004). Lake Issyk-Kul (Tien Shan): Unusually low heat flow in an active intermontane basin. Geol. geofiz. (Novosib.) 45(5): 616-625
In: Геология и Геофизика = Geologiya I Geofizika. Nauka, Sibirskoe otdelenie: Novosibirsk. ISSN 0016-7886
|
| Author keywords |
Heat flow geothermal gradients geodynamical models Lake Issyk Kul’ Tien Shan Kyrghyzstan |
| Auteurs | | Top |
- Vermeesch, P.
- Poort, J.
- Duchkov, A. D.
|
|
|
| Abstract |
New geothermal data are presented for Lake Issyk Kul’, a mountain lake in the northern Tien Shan, Central Asia. With 40 successful measurements done, the average heat flow is 48.3 mW/m2. This is 10 to 20 mW/m2 lower than estimates from previous surveys. Data from boreholes on the shores of the lake revealed an average heat flow of 54 mW/m2. All these values are remarkably low for an actively deforming area such as the Tien Shan. Two qualitative geodynamical models are suggested to explain these observations. If there is crustal thickening beneath Issyk Kul’, the low heat flow can only be explained in a transient mode, with “sawtooth geotherm”. In equilibrium conditions, low heat flow implies that there is little or no crustal thickening under the basin. This feature could be the result of lithospheric folding, as may occur throughout Central Asia. |
IMIS is ontwikkeld en wordt gehost door het VLIZ.
