div class=ts-pagebuttonPage 1button div class=ts-image a href=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5page1jpg target=_blank amp-img class=ts-thumb alt=Page 1: la · leetiv de hidrogeologi din cadrul APGG con- düsrdè G Simion Cretacicul inferior îmbracä douä faciesuri distincte in cele douä zone de sedimentare In versantu} src=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5thumbnails1jpg width=142 height=106 layout=responsive amp-imga divpwwwkarstgeologycompdivdiv class=ts-pagebuttonPage 2button div class=ts-image a href=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5page2jpg target=_blank amp-img class=ts-thumb alt=Page 2: la · leetiv de hidrogeologi din cadrul APGG con- düsrdè G Simion Cretacicul inferior îmbracä douä faciesuri distincte in cele douä zone de sedimentare In versantu} src=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5thumbnails2jpg width=142 height=106 layout=responsive amp-imga divpwwwkarstgeologycompdivdiv class=ts-pagebuttonPage 3button div class=ts-image a href=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5page3jpg target=_blank amp-img class=ts-thumb alt=Page 3: la · leetiv de hidrogeologi din cadrul APGG con- düsrdè G Simion Cretacicul inferior îmbracä douä faciesuri distincte in cele douä zone de sedimentare In versantu} src=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5thumbnails3jpg width=142 height=106 layout=responsive amp-imga divpwwwkarstgeologycompdivdiv class=ts-pagebuttonPage 4button div class=ts-image a href=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5page4jpg target=_blank amp-img class=ts-thumb alt=Page 4: la · leetiv de hidrogeologi din cadrul APGG con- düsrdè G Simion Cretacicul inferior îmbracä douä faciesuri distincte in cele douä zone de sedimentare In versantu} src=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5thumbnails4jpg width=142 height=106 layout=responsive amp-imga divpwwwkarstgeologycompdivdiv class=ts-pagebuttonPage 5button div class=ts-image a href=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5page5jpg target=_blank amp-img class=ts-thumb alt=Page 5: la · leetiv de hidrogeologi din cadrul APGG con- düsrdè G Simion Cretacicul inferior îmbracä douä faciesuri distincte in cele douä zone de sedimentare In versantu} src=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5thumbnails5jpg width=142 height=106 layout=responsive amp-imga divpwwwkarstgeologycompdivdiv class=ts-pagebuttonPage 6button div class=ts-image a href=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5page6jpg target=_blank amp-img class=ts-thumb alt=Page 6: la · leetiv de hidrogeologi din cadrul APGG con- düsrdè G Simion Cretacicul inferior îmbracä douä faciesuri distincte in cele douä zone de sedimentare In versantu} src=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5thumbnails6jpg width=142 height=106 layout=responsive amp-imga divpwwwkarstgeologycompdivdiv class=ts-pagebuttonPage 7button div class=ts-image a href=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5page7jpg target=_blank amp-img class=ts-thumb alt=Page 7: la · leetiv de hidrogeologi din cadrul APGG con- düsrdè G Simion Cretacicul inferior îmbracä douä faciesuri distincte in cele douä zone de sedimentare In versantu} src=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5thumbnails7jpg width=142 height=106 layout=responsive amp-imga divpwwwkarstgeologycompdivdiv class=ts-pagebuttonPage 8button div class=ts-image a href=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5page8jpg target=_blank amp-img class=ts-thumb alt=Page 8: la · leetiv de hidrogeologi din cadrul APGG con- düsrdè G Simion Cretacicul inferior îmbracä douä faciesuri distincte in cele douä zone de sedimentare In versantu} src=https:reader042vdocumentecomreader042viewer20220315045c85652f09d3f2ea4b8c7e94html5thumbnails8jpg width=142 height=106 layout=responsive amp-imga divpwwwkarstgeologycompdiv