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dc.contributor.authorKevin P Furlongen_US
dc.date.accessioned2020-04-02T14:45:04Z-
dc.date.available2020-04-02T14:45:04Z-
dc.date.issued2020en_US
dc.identifier.citationChiang Mai Journal of Science 43, 6 (Special Issue - December 2016), 1223-1236en_US
dc.identifier.issn0125-2526en_US
dc.identifier.urihttp://epg.science.cmu.ac.th/ejournal/dl.php?journal_id=7604en_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/67350-
dc.description.abstractTemperature conditions in the crust control many geologic processes. Careful incorporation of the thermal field can provide additional constraints on geologic and geophysical analyses. The basics of crustal and lithospheric thermal structure are discussed and two examples of application of thermal modeling for mountainy building and basin evolution are provided.en_US
dc.language.isoEngen_US
dc.publisherScience Faculty of Chiang Mai Universityen_US
dc.subjectheat flowen_US
dc.subjectgeotherm thermochronologyen_US
dc.titleFrom Mountain Heights to Basin Depths: The Importance of Thermal Geophysics in Tectonics, Seismology, and Petroleum Geoscienceen_US
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