Amenable 发表于 2025-3-25 03:30:03
http://reply.papertrans.cn/29/2811/281077/281077_21.pngAerate 发表于 2025-3-25 11:03:39
Jean Guex,Federico Galster,Øyvind HammerPresents the summary of quantitative construction of discrete paleontological timescales.Offers numerous applications for paleontologists and geologists.Includes models related to important mass extin等待 发表于 2025-3-25 15:34:24
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http://reply.papertrans.cn/29/2811/281077/281077_24.pngCertainty 发表于 2025-3-25 20:03:44
Reliability-Based Design Optimizationabama Geol Surv Bull 80:1–84, .). The goal of Deboo was two-fold: first, he intended to solve some problems posed by correlating the lithologic units classically used in this region (Fig. .) and second, he wanted to use new biochronologic arguments to determine more precisely the boundary between thaccrete 发表于 2025-3-26 01:03:05
https://doi.org/10.1007/978-3-030-12819-7 from 32 Neogene sections around the Southern Ocean and Antarctic continental margin has been recently studied by Cody et al. (Palaeogeogr Palaeoclimatol Palaeoecol 260:92–121, .). A new method, known as Constrained Optimization (Conop), which can be viewed as a multidimensional version of graphic c者变 发表于 2025-3-26 06:15:48
https://doi.org/10.1007/978-3-031-23898-7o proceed to such a calibration we need essentially to use marine time diagnostic fossils like Graptolites, Trilobites, Ammonites or planctonic Foraminifera associated with coeval volcanic ashes or lava flows containing radiogenic minerals like zircons for U-Pb dating or K-feldspars for Ar–Ar datingtackle 发表于 2025-3-26 08:44:48
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e use of highly efficient software along with several examples. The authors compare their theoretical model with 2 other relevant studies: probabilistic stratigraphy and constrained optimization (CONOP)..978-3-319-37272-3978-3-319-21326-2Adornment 发表于 2025-3-26 18:24:31
d geologists.Includes models related to important mass extin.The object of this book is to explain how to create a synthesis of complex biostratigraphic data, and how to extract from such a synthesis a relative time scale based exclusively on the fossil content of sedimentary rocks. Such a time scal