{"refrec":{"BRefID":23594,"RR":"<b>Delisle, G.; Beiersdorf, H.; Neben, S.; Steinmann, D.</b> (1998). The geothermal field of the North Sulawesi accretionary wedge and a model on BSR migration in unstable depositional environments, <b><i>in</i></b>: Henriet, J.-P. <i>et al.</i> <i>Gas hydrates: relevance to world margin stability and climate change. Geological Society Special Publication,</i> 137: pp. 267-274. <a href=\"https://dx.doi.org/10.1144/GSL.SP.1998.137.01.21\" target=\"_blank\">https://dx.doi.org/10.1144/GSL.SP.1998.137.01.21</a>","BEntID":23594,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":", <b><i>in</i></b>: Henriet, J.-P. <i>et al.</i> <i>Gas hydrates: relevance to world margin stability and climate change. Geological Society Special Publication,</i> 137: pp. 267-274. <a href=\"https://dx.doi.org/10.1144/GSL.SP.1998.137.01.21\" target=\"_blank\">https://dx.doi.org/10.1144/GSL.SP.1998.137.01.21</a>","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Delisle, G.; Beiersdorf, H.; Neben, S.; Steinmann, D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Delisle, G. <i>et al.</i>","Englishabstract":"The distribution of heat flow in the North Sulawesi accretionary wedge was derived from the depths of a bottom simulating reflector (BSR) and nine <em>in situ</em> heat flow measurements. The values obtained by both types of measurements agree reasonably well and suggest high heat flow of the order of 70–100 mW m<sup>−2</sup> near the deformation front and a systematic decrease to 30 mW m<sup>−2</sup> landwards. In addition, we have tested on the basis of one numerical model the likelihood of the BSR being in a position of complete thermal equilibrium with the surrounding rocks. The model describes the rate by which a BSR layer re-equilibrates after a thermal disturbance at the sea floor (sediment slumping). The result suggests that the BSR does not regain complete thermal equilibrium after slumping in the course of several 10<sup>5</sup> years.","AbstractOtherLang":null,"BibLvlCode":"AMS","StandardTitle":"The geothermal field of the North Sulawesi accretionary wedge and a model on BSR migration in unstable depositional environments","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2025-07-02 08:33:14.980000","timezone_type":1,"timezone":"+00:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":"accretionary wedge, BSR migration","Notes":null,"AnaPub":1998,"MonPub":null,"DateUpdate":"2022-03-22","DateCreate":"2002-03-21","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0,"DOI":"10.1144/GSL.SP.1998.137.01.21"},"refs":null,"anarec":{"AnaID":23594,"PubliDate":1998,"Pagination":"267-274","XtraPublOfAnaID":null,"ISBN":"1-86239-010-X","Volume":"137","Issue":null,"BRefMon":23545,"BRefMonRR":"<b>Henriet, J.-P.; Mienert, J.</b> (1998). 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