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作 者:G.Shanmugam
机构地区:[1]Department of Earth and Environmental Sciences,The University of Texas at Arlington
出 处:《Journal of Palaeogeography》2017年第3期224-234,共11页古地理学报(英文版)
摘 要:This discussion of a paper by Van Loon et al.(2016), published in the Journal of Palaeogeography(2016, 5(4), 381e390), is aimed at illustrating that there are fundamental deficiencies, which include(1)incomplete etymological reasoning for proposing a new genetic term "tomboliths" for stromatolitic bioclasts in the Palaeoproterozoic Chaibasa Formation, eastern India,(2) omission of empirical data in documenting depositional facies using sedimentological logs,(3) misapplication of the stratigraphic concept of "angular unconformity",(4) failure to consider the multifarious origins of earthquakes, and(5) a dated view on the basic tenets of process sedimentology and triggering mechanisms of liquefaction that are the basis for forming soft-sediment deformation structures(SSDS). As a consequence, their conclusions are unconvincing.This discussion of a paper by Van Loon et al.(2016), published in the Journal of Palaeogeography(2016, 5(4), 381e390), is aimed at illustrating that there are fundamental deficiencies, which include(1)incomplete etymological reasoning for proposing a new genetic term "tomboliths" for stromatolitic bioclasts in the Palaeoproterozoic Chaibasa Formation, eastern India,(2) omission of empirical data in documenting depositional facies using sedimentological logs,(3) misapplication of the stratigraphic concept of "angular unconformity",(4) failure to consider the multifarious origins of earthquakes, and(5) a dated view on the basic tenets of process sedimentology and triggering mechanisms of liquefaction that are the basis for forming soft-sediment deformation structures(SSDS). As a consequence, their conclusions are unconvincing.
关 键 词:Stromatolitic bioclasts Seismic shocks Soft-sediment deformation structures(SSDS) Palaeoproterozoic Chaibasa Formation Singhbhum Craton Eastern India
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