<> "The repository administrator has not yet configured an RDF license."^^ . <> . . "Controlling factors of two Middle Triassic carbonate platforms: Latemar and Rosengarten (Dolomites, Northern Italy)"^^ . "Integrated facies and subsidence analysis enable the identification and quantification of controlling factors on carbonate platform evolution. Palaeo biologic evolution as intrinsic factors, subsidence and accommodation change as extrinsic factors are the most important controlling factors on carbonate platform growth on a platform (and basin)-wide scale. Other factors like auto-cyclic processes, windward-leeward effects, nutrient supply, wave expositions and tidal currents are also important but play a minor, localised role. Whereas subsidence and accommodation change can easily be deduced from the sedimentary record and be quantitatively assessed, the other factors are much more difficult to identify lest quantify due to overprinting and poor preservation potential. Facies analysis and the comparison of the slope- and reef-facies from Latemar (Upper Anisian/Lower Ladinian, Dolomites) and Concarena (Upper Ladinian/Lower Carnian, Lombardic Alps) stresses the importance and links between subsidence, sedimentation, facies assemblages and cementation throughout the development of Triassic carbonate platforms. High rates of carbonate accumulation/accommodation increase combined with low topography of the reefal margin prevent massive early cementation at Latemar; low rates during the last stages of the Concarena platform together with a walled reef promote massive early cementation. Combined thermal, numerical basin reverse and sequence stratigraphic forward modelling constrained burial and subsidence histories of the Rosengarten and Latemar platforms. Vitrinite reflectance and apatite fission track data both argue for a shallow maximum burial. Present day topography was overlain by a maximum thickness of 1100m of overburden. There are no indications for a Neogene flysch or molasse-type setting as inferred from other Alpine basins. The subsidence pulse at the verge of the Anisian (Reitzi-zone) is recorded at Latemar and Rosengarten with similar total subsidence rates of 800-850m/Ma. Both platforms successfully kept up with this rapid increase in accommodation space. Additionally, sequence stratigraphic forward modelling of the Rosengarten platform showed that minimum vertical accumulation rates of up to 1000m/Ma are necessary in order to reproduce observed present day geometries. The carbonate production rates of both platforms reached values of (sub)recent carbonate platforms. Despite the resemblance of the Latemar reef to other early Anisian reefs of the Dolomites (encrusting microproblematica dominating over framebuilding organisms) and the low diversity of faunal elements with respect to slightly younger reefs (e.g. Concarena, Ladinian/Carnian), this adds further evidence to the observation of a full recovery of the carbonate factory already at the Late Anisian (lower Middle Triassic)."^^ . "2004" . . . . . . . . "Axel"^^ . "Emmerich"^^ . "Axel Emmerich"^^ . . . . . . "Controlling factors of two Middle Triassic carbonate platforms: Latemar and Rosengarten (Dolomites, Northern Italy) (PDF)"^^ . . . "ae04low.pdf"^^ . . . "Controlling factors of two Middle Triassic carbonate platforms: Latemar and Rosengarten (Dolomites, Northern Italy) (Other)"^^ . . . . . . "small.jpg"^^ . . . "Controlling factors of two Middle Triassic carbonate platforms: Latemar and Rosengarten (Dolomites, Northern Italy) (Other)"^^ . . . . . . "medium.jpg"^^ . . . "Controlling factors of two Middle Triassic carbonate platforms: Latemar and Rosengarten (Dolomites, Northern Italy) (Other)"^^ . . . . . . "preview.jpg"^^ . . . "Controlling factors of two Middle Triassic carbonate platforms: Latemar and Rosengarten (Dolomites, Northern Italy) (Other)"^^ . . . . . . "lightbox.jpg"^^ . . "HTML Summary of #4791 \n\nControlling factors of two Middle Triassic carbonate platforms: Latemar and Rosengarten (Dolomites, Northern Italy)\n\n" . "text/html" . . . "550 Geowissenschaften"@de . "550 Earth sciences"@en . .