div class=trans-pagebuttonPage 1button div class=trans-image amp-img class=trans-thumb 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 src=https:reader036fdocumentsnetreader036viewer20220712186051d6da8110b4085536176ahtml5thumbnails1jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 2button div class=trans-image amp-img class=trans-thumb 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 src=https:reader036fdocumentsnetreader036viewer20220712186051d6da8110b4085536176ahtml5thumbnails2jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 3button div class=trans-image amp-img class=trans-thumb 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 src=https:reader036fdocumentsnetreader036viewer20220712186051d6da8110b4085536176ahtml5thumbnails3jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 4button div class=trans-image amp-img class=trans-thumb alt=Page 4: 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 src=https:reader036fdocumentsnetreader036viewer20220712186051d6da8110b4085536176ahtml5thumbnails4jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 5button div class=trans-image amp-img class=trans-thumb alt=Page 5: 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...