作者: Fernando Flávio Marques De Almeida , Celso Dal Ré Carneiro
关键词:
摘要: The origin of the subparallel mountain systems which compose coastal Serra do Mar and inland da Mantiqueira is related to Upper Cretaceous. These features - distributed along a quite singular continental atlantic border nave complex evolution arising controversial questions. answers these problems are mainly dependentto dating Japi erosional surface other younger ones, study still faced by small amount detailed-scale surveys. scarp domains covered dense vegetation often impose difficult trail access. Nevertheless, present knowledge stage allows us admit that during Tertiary local relief has affected into considerable extent synchronic oceanic phase sediments Santos Basin. There lot evidence proofs been developed from very different geographical position as compared existing one. hypothesis supported authors long-term retreat southeast northwest due processes approximately starting at fault line in platform.