div class=ts-pagebutton class=gotoPage data-page=1Page 1button div class=ts-imageimg data-url=powerpoint-presentation-2-temperature-of-lithosphere-derived-from-half-space-coolinghtmlpage=1 data-page=1 class=ts-thumb lazyload alt=Page 1: PowerPoint Presentation2 Temperature of lithosphere derived from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails1jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=2Page 2button div class=ts-imageimg data-url=powerpoint-presentation-2-temperature-of-lithosphere-derived-from-half-space-coolinghtmlpage=2 data-page=2 class=ts-thumb lazyload alt=Page 2: PowerPoint Presentation2 Temperature of lithosphere derived from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails2jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=3Page 3button div class=ts-imageimg data-url=powerpoint-presentation-2-temperature-of-lithosphere-derived-from-half-space-coolinghtmlpage=3 data-page=3 class=ts-thumb lazyload alt=Page 3: PowerPoint Presentation2 Temperature of lithosphere derived from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails3jpg 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from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails5jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=6Page 6button div class=ts-imageimg data-url=powerpoint-presentation-2-temperature-of-lithosphere-derived-from-half-space-coolinghtmlpage=6 data-page=6 class=ts-thumb lazyload alt=Page 6: PowerPoint Presentation2 Temperature of lithosphere derived from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC 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of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails12jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=13Page 13button div class=ts-imageimg data-url=powerpoint-presentation-2-temperature-of-lithosphere-derived-from-half-space-coolinghtmlpage=13 data-page=13 class=ts-thumb lazyload alt=Page 13: PowerPoint Presentation2 Temperature of lithosphere derived from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails13jpg width=140 height=200 divdivdiv class=ts-pagebutton 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depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails15jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=16Page 16button div class=ts-imageimg data-url=powerpoint-presentation-2-temperature-of-lithosphere-derived-from-half-space-coolinghtmlpage=16 data-page=16 class=ts-thumb lazyload alt=Page 16: PowerPoint Presentation2 Temperature of lithosphere derived from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails16jpg width=140 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from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails18jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=19Page 19button div class=ts-imageimg data-url=powerpoint-presentation-2-temperature-of-lithosphere-derived-from-half-space-coolinghtmlpage=19 data-page=19 class=ts-thumb lazyload alt=Page 19: PowerPoint Presentation2 Temperature of lithosphere derived from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC 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bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails22jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=23Page 23button div class=ts-imageimg data-url=powerpoint-presentation-2-temperature-of-lithosphere-derived-from-half-space-coolinghtmlpage=23 data-page=23 class=ts-thumb lazyload alt=Page 23: PowerPoint Presentation2 Temperature of lithosphere derived from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails23jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage 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exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails25jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=26Page 26button div class=ts-imageimg data-url=powerpoint-presentation-2-temperature-of-lithosphere-derived-from-half-space-coolinghtmlpage=26 data-page=26 class=ts-thumb lazyload alt=Page 26: PowerPoint Presentation2 Temperature of lithosphere derived from half-space cooling model 3 Viscosity depends exponentially on temperature contrast of 1015 viscosity bounds loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader033vdocumentinreader033viewer20220530045f08236d7e708231d4208766html5thumbnails26jpg width=140 height=200 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