div class=trans-pagebutton class=gotoPage data-page=1Page 1button div class=trans-imageimg data-url=documentuniversitt-innsbruck-eberli-et-al-that-were-uplifted-later-by-alpine-thrustinghtmlpage=1 data-page=1 class=trans-thumb lazyload alt=Page 1: Universität Innsbruck · Eberli et al that were uplifted later by Alpine thrusting and folding Typically platform margins have been sites of tectonic decoupling during orogeny loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAEAAAABCAQAAAC1HAwCAAAAC0lEQVR42mM8Uw8AAh0BTZud3BwAAAAASUVORK5CYII= data-src=https:reader036fdocumentsnetreader036viewer20220712186051d6da8110b4085536176ahtml5thumbnails1jpg width=140 height=200 divdivdiv class=trans-pagebutton class=gotoPage data-page=2Page 2button div class=trans-imageimg data-url=documentuniversitt-innsbruck-eberli-et-al-that-were-uplifted-later-by-alpine-thrustinghtmlpage=2 data-page=2 class=trans-thumb lazyload alt=Page 2: Universität Innsbruck · Eberli et al that were uplifted later by Alpine thrusting and folding Typically platform margins have been sites of tectonic decoupling during orogeny loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAEAAAABCAQAAAC1HAwCAAAAC0lEQVR42mM8Uw8AAh0BTZud3BwAAAAASUVORK5CYII= data-src=https:reader036fdocumentsnetreader036viewer20220712186051d6da8110b4085536176ahtml5thumbnails2jpg width=140 height=200 divdivdiv class=trans-pagebutton class=gotoPage data-page=3Page 3button div class=trans-imageimg data-url=documentuniversitt-innsbruck-eberli-et-al-that-were-uplifted-later-by-alpine-thrustinghtmlpage=3 data-page=3 class=trans-thumb lazyload alt=Page 3: Universität Innsbruck · Eberli et al that were uplifted later by Alpine thrusting and folding Typically platform margins have been sites of tectonic decoupling during orogeny loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAEAAAABCAQAAAC1HAwCAAAAC0lEQVR42mM8Uw8AAh0BTZud3BwAAAAASUVORK5CYII=...