The Poso Depression provides a record of Plio-Pleistocene environments and palaeogeography of Central Sulawesi.Outcrop-based sedimentological and provenance studies suggest that during the Pliocene the Poso Depression...The Poso Depression provides a record of Plio-Pleistocene environments and palaeogeography of Central Sulawesi.Outcrop-based sedimentological and provenance studies suggest that during the Pliocene the Poso Depression was a sea channel connecting Gorontalo and Bone bays formed in an asymmetric half-graben.The Pliocene history began with deposition of the Puna Formation with fan deltas at the eastern basin margin and channel complexes in the deep-water basin further east.Analyses of light and heavy minerals indicate the main sediment source was ultrabasic rocks in East Sulawesi with minor and intermittent magmatic and metamorphic input from West Sulawesi.Later,in the Middle to Late Pliocene,carbonates of the Poso Formation accumulated on the eastern basin margin.They are unconformably overlain by shallow marine glaucophane-rich siliciclastics of the Pleistocene Lage Formation that are associated with the rapid exhu-mation and uplift of the Pompangeo metamorphic complex.This uplift led to the development of a land bridge connecting western and eastern Sulawesi.The terrane evolution favoured increasing the area of exposed land due to rapid tectonic uplift,which when combined with the tropical climate,contributed to faunal speciation and dispersal in Sulawesi.展开更多
基金supported by the SE Asia Research Group of Royal Holloway University of London,United Kingdom,which is backed by a consortium of oil companiessupported by the Earth Observatory of Singapore(EOS),Singapore and comprises EOS contribution number 508
文摘The Poso Depression provides a record of Plio-Pleistocene environments and palaeogeography of Central Sulawesi.Outcrop-based sedimentological and provenance studies suggest that during the Pliocene the Poso Depression was a sea channel connecting Gorontalo and Bone bays formed in an asymmetric half-graben.The Pliocene history began with deposition of the Puna Formation with fan deltas at the eastern basin margin and channel complexes in the deep-water basin further east.Analyses of light and heavy minerals indicate the main sediment source was ultrabasic rocks in East Sulawesi with minor and intermittent magmatic and metamorphic input from West Sulawesi.Later,in the Middle to Late Pliocene,carbonates of the Poso Formation accumulated on the eastern basin margin.They are unconformably overlain by shallow marine glaucophane-rich siliciclastics of the Pleistocene Lage Formation that are associated with the rapid exhu-mation and uplift of the Pompangeo metamorphic complex.This uplift led to the development of a land bridge connecting western and eastern Sulawesi.The terrane evolution favoured increasing the area of exposed land due to rapid tectonic uplift,which when combined with the tropical climate,contributed to faunal speciation and dispersal in Sulawesi.
