TIMING AND MECHANISMS OF TERMINATION OF THE INTERIOR OF A SHALLOW MARINE CARBONATE PLATFORM: THE PINGGUO PLATFORM, NANPANJIANG BASIN, GUANGXI PROVINCE, SOUTH CHINA

The Pingguo platform is one of several isolated Triassic platforms in the Nanpanjiang Basin, a rapidly subsiding embayment in the Yangtze microcontinent of the equatorial eastern Tethys. The Pingguo platform evolved from a low-relief bank followed by vast areas of platform interior termination (step back) and development of smaller pinnacle platforms. Three sections were measured through the termination interval in a NW cross-section. The vertical facies pattern consists of: 1) molluscan dolowackestone-packstone with microbial laminites and fenestrae, 2) an interval with numerous mineralized and bored hardgrounds, 3) thick-bedded, dark-gray molluscan and oncolitic wackestone-mudstone, followed by 4) dark, organic-rich, nodular-bedded, and laminated lime mudstones containing echinoderms, ammonoids, conodonts, and radiolarians, and 5) shale. Facies (1) occurs in the uppermost shallow-subtidal portion of the carbonate platform and contains features consistent with restricted subtidal to intertidal conditions. Deepening and "stalling" of carbonate productivity are indicated by the hardgrounds in facies (2) and the dark gray color of facies (3) which may have been deposited between normal and storm wave-base. Shifting to deep, sub-photic conditions, shut down of carbonate productivity, and termination of the platform interior are indicated by the features and pelagic fossils in facies (4). Termination of the interior occurred during the Early Anisian (Aegean) as indicated by the conodonts Neospathodus abruptus, Neogondolella regale, and the ammonoids Bulogites, and Paraceratites. The facies succession indicates the platform was terminated by drowning below the photic zone by a combination of subsidence and sea level rise. Siliciclastic flux is not the primary cause because facies indicate deepening conditions long before shale interbeds occur. Nodular-bedded and laminated lime mudstones of the termination interval are relatively argillaceous resulting from shut down in carbonate productivity and concentration of background siliciclastics. Documentation of the interior termination and bank to pinnacle architecture of the Pingguo platform is important for understanding regional patterns in differential tectonic subsidence and platform evolution across the basin.