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Titlebook: Discrete Biochronological Time Scales; Jean Guex,Federico Galster,?yvind Hammer Book 2016 Springer International Publishing Switzerland 20

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樓主: 傳家寶
21#
發(fā)表于 2025-3-25 03:30:03 | 只看該作者
22#
發(fā)表于 2025-3-25 11:03:39 | 只看該作者
Jean Guex,Federico Galster,?yvind HammerPresents the summary of quantitative construction of discrete paleontological timescales.Offers numerous applications for paleontologists and geologists.Includes models related to important mass extin
23#
發(fā)表于 2025-3-25 15:34:24 | 只看該作者
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25#
發(fā)表于 2025-3-25 20:03:44 | 只看該作者
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 th
26#
發(fā)表于 2025-3-26 01:03:05 | 只看該作者
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
27#
發(fā)表于 2025-3-26 06:15:48 | 只看該作者
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 dating
28#
發(fā)表于 2025-3-26 08:44:48 | 只看該作者
29#
發(fā)表于 2025-3-26 16:16:09 | 只看該作者
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)..978-3-319-37272-3978-3-319-21326-2
30#
發(fā)表于 2025-3-26 18:24:31 | 只看該作者
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
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