机译:来自东北皮尔巴拉克拉通的太古代推定微化石的三维形态和质地复杂性:大型(>15μm)球形和纺锤状结构的生物成因指示
Department of Environmental Engineering and Architecture Graduate School of Environmental Studies Nagoya University Nagoya 464-8601 Japan;
Geological Survey of Western Australia, Department of Mines and Petroleum, East Perth, Australia Australian Centre for Astrobiology, University of New South Wales, Sydney, Australia;
School of Informatics and Sciences, Nagoya University, Nagoya, Japan;
Department of Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan;
archean; microfossil; pilbara craton; mount goldsworthy-mount grant; in-focus and 3-D images;
机译:西澳大利亚州Pilbara Craton东北部Goldsworthy-Mount Grant地区的古生球状微化石(约3.0 Ga)的分类学和生物成因
机译:来自西澳大利亚州Pilbara Craton的Mount Grant地区的太古代微化石(约3.0 Ga)的孢粉学:生物成因的进一步证据
机译:在皮尔巴拉克拉通山戈德斯沃西山绿岩带上的太古代石的系统化稀土元素和钇研究:含微化石的黑色石起源的启示
机译:作为来自西澳大利亚Pilbara Craton的3.5-3.2 Ga Fossil Stromatolites的生物发生指标。
机译:导电性孵化与Archean Grante-Greenstone Terrains中的圆顶和龙骨结构的起源:基于西澳大利亚西部的西部Pilbara Craton的模型