scholarly journals Supplemental Material: Cretaceous to Oligocene magmatic and tectonic evolution of the western Alaska Range: Insights from U-Pb and 40Ar/39Ar geochronology

2020 ◽  
Author(s):  
J.V. Jones III ◽  
et al.

<div>Complete descriptions of all U-Pb and <sup>40</sup>Ar/<sup>39</sup>Ar analytical methods together with detailed analytical data for all samples.<br></div><div><br></div><div><br></div><div><br></div>

2020 ◽  
Author(s):  
J.V. Jones III ◽  
et al.

<div>Complete descriptions of all U-Pb and <sup>40</sup>Ar/<sup>39</sup>Ar analytical methods together with detailed analytical data for all samples.<br></div><div><br></div><div><br></div><div><br></div>


Minerals ◽  
2021 ◽  
Vol 11 (6) ◽  
pp. 604
Author(s):  
Evgeny V. Vetrov ◽  
Johan De Grave ◽  
Natalia I. Vetrova ◽  
Fedor I. Zhimulev ◽  
Simon Nachtergaele ◽  
...  

The West Siberian Basin (WSB) is one of the largest intracratonic Meso-Cenozoic basins in the world. Its evolution has been studied over the recent decades; however, some fundamental questions regarding the tectonic evolution of the WSB remain unresolved or unconfirmed by analytical data. A complete understanding of the evolution of the WSB during the Mesozoic and Cenozoic eras requires insights into the cooling history of the basement rocks as determined by low-temperature thermochronometry. We presented an apatite fission track (AFT) thermochronology study on the exposed parts of the WSB basement in order to distinguish tectonic activation episodes in an absolute timeframe. AFT dating of thirteen basement samples mainly yielded Cretaceous cooling ages and mean track lengths varied between 12.8 and 14.5 μm. Thermal history modeling based on the AFT data demonstrates several Mesozoic and Cenozoic intracontinental tectonic reactivation episodes affected the WSB basement. We interpreted the episodes of tectonic activity accompanied by the WSB basement exhumation as a far-field effect from tectonic processes acting on the southern and eastern boundaries of Eurasia during the Mesozoic–Cenozoic eras.


2002 ◽  
Vol 74 (12) ◽  
pp. 2281-2291 ◽  
Author(s):  
H. H. Hill ◽  
S. J. Martin

Analytical methods that are currently used for the detection and identification of chemical warfare agents are reviewed and classified by the number of dimensions of information they provide. Single dimensional sensors target specific compounds or classes of compounds. Although they can be less expensive and more portable than multidimensional sensors, multidimensional sensors detect a broader threat spectrum with greater precision and accuracy. The recommendation for analytical field verification during inspections under the Chemical Weapons Convention (CWC) is to use simple two-dimensional analytical methods, such as gas chromatography (GC) or ion mobility spectrometry (IMS), for on-site screening of chemical weapons (CW) agents or to fully equip a modern, mobile analytical laboratory located in an airplane, which can be moved rapidly throughout the world to each inspection site and provide high-quality analytical data on-site.


2021 ◽  
Author(s):  
Jared T. Gooley ◽  
et al.

Appendix S1: Geologic map data sources; Appendix S2: Sample preparation and analytical methods; Table S1: U-Th-Pb data; Table S2: U-Pb age components.


1994 ◽  
Vol 29 (3) ◽  
pp. 69-76 ◽  
Author(s):  
Hubert Hellmann

The period between 1955 and 1988 was the time of reconstruction in the destroyed Federal Republic of Germany, marked by booming industrial development and - with some delay -by the rise and spread of ecological awareness and the idea of water conservation. This is the background against which the analysis of water quality and of pollution load trends should be seen. The study of a long-term load trend presupposes the following requirements:–sufficiently large number of measured data;–reliable, reproducible analytical methods which produce comparable results over long time series; and–hydrological interpretation and evaluation of results. The continuous efforts to improve analytical methods and the elimination of distorting substances and matrix effects led to the situation that long time series of data are not directly comparable. In some cases, summative analyses (aggregate parameters) have been replaced by newly developed substance-specific methods so that the continuity of records has been broken. Furthermore, there is a general underestimation of the necessity to consider and evaluate analytical data in a space-time continuum. However, on the whole, we are able to give a satisfying interpretation of trends for the classical parameters. In the case of the trace substances detected by modem methods, this is possible only for the past two decades and with some reservations.


2021 ◽  
Author(s):  
◽  

This Open-File Report makes available raw analytical data from laboratory procedures completed to determine the age of a rock sample collected during geologic investigations funded or partially supported by the Utah Geological Survey (UGS). Table 1 provides the sample identification and location for the age data. The references listed in table 1 generally provide additional information such as sample location, geologic setting, and significance or interpretation of the sample in the context of the area where it was collected. This report was prepared by Krueger Enterprises, Inc., Geochron Laboratories Division in 1995 under contract to the UGS. These data are highly technical in nature and proper interpretation requires considerable training in the applicable geochronologic techniques.


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