| | GFF-online presents: Transgressive oolites onlapping a Silurian rocky shoreline unconformity, Gotland, Sweden (Site not responding. Last check: 2007-11-07) |
 | | The major facies-elements forming the rocky shoreline are 1) several subaerially exposed reefs, which were eroded during falling base-level and which form the topography, and 2), onlap of oolite grainstones which were deposited during the subsequent rise of the base-level. |
 | | Five localities along the rocky shoreline are discussed in detail here, viz., Svalings 1 where the unconformable boundary is accessible, and Bara 1-4 where the petrography of the onlapping oolite has been studied. |
 | | The Slite Rocky Shoreline Unconformity (SRSU) is herein considered as the platform-proximal equivalent to the sequence boundary separating the regressive Fröjel Formation and the transgressive Bara Oolite Member (lowermost Halla Formation) in the Klintehamn area on western Gotland. |
| www.gff-online.se /site/article.asp?articleID=493 (379 words) |