Abstract
We analyze available heat flow data from the flanks of the Southeast Indian Ridge adjacent to or within the Australian‐Antarctic Discordance (AAD), an area with patchy sediment cover and highly fractured seafloor as dissected by ridge‐ and fracture‐parallel faults. The data set includes 23 new data points collected along a 14‐Ma old isochron and 19 existing measurements from the 20‐ to 24‐Ma old crust. Most sites of measurements exhibit low heat flux (from 2 to 50 mW m−2) with near‐linear temperature‐depth profiles except at a few sites, where recent bottom water temperature change may have caused nonlinearity toward the sediment surface. Because the igneous basement is expected to outcrop a short distance away from any measurement site, we hypothesize that horizontally channelized water circulation within the uppermost crust is the primary process for the widespread low heat flow values. The process may be further influenced by vertical fluid flow along numerous fault zones that crisscross the AAD seafloor. Systematic measurements along and across the fault zones of interest as well as seismic profiling for sediment distribution are required to confirm this possible, suspected effect.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.