Structural characterization of kerogen in 3.4 Ga Archaean
Hydrogen-lean kerogen (atomic H/C < 0.46) isolated from the 3.4 Ga Strelley Pool Chert in the North Pole area, Pilbara Craton, Western Australia, were studied by vibrational spectroscopy (Fourier transform infrared (FTIR) spectroscopy and Raman spectroscopy), nuclear magnetic resonance spectrosco...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.207.468 2023-05-15T17:39:47+02:00 Structural characterization of kerogen in 3.4 Ga Archaean Western Australia Craig P. Marshall A Gordon D. Love C Colin E. Snape E Andrew C. Hill F Abigail C. Allwood B Malcolm R. Walter B Martin J. Van Kranendonk G Stephen A. Bowden H Sean P. Sylva I Roger E. Summons C The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.207.468 http://earthsciences.ucr.edu/docs/Marshall%20et%20al%20%202007%20(2).pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.207.468 http://earthsciences.ucr.edu/docs/Marshall%20et%20al%20%202007%20(2).pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://earthsciences.ucr.edu/docs/Marshall%20et%20al%20%202007%20(2).pdf text ftciteseerx 2016-01-07T17:41:17Z Hydrogen-lean kerogen (atomic H/C < 0.46) isolated from the 3.4 Ga Strelley Pool Chert in the North Pole area, Pilbara Craton, Western Australia, were studied by vibrational spectroscopy (Fourier transform infrared (FTIR) spectroscopy and Raman spectroscopy), nuclear magnetic resonance spectroscopy (solid state 13 C NMR spectroscopy), catalytic hydropyrolysis followed by gas chromatography mass spectrometry (HyPy–GC–MS), and isotope ratio mass spectrometry (IRMS). The kerogen occurs in sedimentary rocks as clasts and clots deposited together with other detrital materials that are finely disseminated throughout a chert matrix. The bulk kerogen δ 13 C values range from −28.3 to −35.8‰. Solid-state 13 C NMR spectroscopy and FTIR spectroscopy reveals that the kerogen is highly aromatic (fa varying from 0.90 to 0.92) and contains only minor aliphatic carbon or carbon-oxygenated (C–O) Text North Pole Unknown North Pole |
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English |
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Hydrogen-lean kerogen (atomic H/C < 0.46) isolated from the 3.4 Ga Strelley Pool Chert in the North Pole area, Pilbara Craton, Western Australia, were studied by vibrational spectroscopy (Fourier transform infrared (FTIR) spectroscopy and Raman spectroscopy), nuclear magnetic resonance spectroscopy (solid state 13 C NMR spectroscopy), catalytic hydropyrolysis followed by gas chromatography mass spectrometry (HyPy–GC–MS), and isotope ratio mass spectrometry (IRMS). The kerogen occurs in sedimentary rocks as clasts and clots deposited together with other detrital materials that are finely disseminated throughout a chert matrix. The bulk kerogen δ 13 C values range from −28.3 to −35.8‰. Solid-state 13 C NMR spectroscopy and FTIR spectroscopy reveals that the kerogen is highly aromatic (fa varying from 0.90 to 0.92) and contains only minor aliphatic carbon or carbon-oxygenated (C–O) |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Western Australia Craig P. Marshall A Gordon D. Love C Colin E. Snape E Andrew C. Hill F Abigail C. Allwood B Malcolm R. Walter B Martin J. Van Kranendonk G Stephen A. Bowden H Sean P. Sylva I Roger E. Summons C |
spellingShingle |
Western Australia Craig P. Marshall A Gordon D. Love C Colin E. Snape E Andrew C. Hill F Abigail C. Allwood B Malcolm R. Walter B Martin J. Van Kranendonk G Stephen A. Bowden H Sean P. Sylva I Roger E. Summons C Structural characterization of kerogen in 3.4 Ga Archaean |
author_facet |
Western Australia Craig P. Marshall A Gordon D. Love C Colin E. Snape E Andrew C. Hill F Abigail C. Allwood B Malcolm R. Walter B Martin J. Van Kranendonk G Stephen A. Bowden H Sean P. Sylva I Roger E. Summons C |
author_sort |
Western Australia |
title |
Structural characterization of kerogen in 3.4 Ga Archaean |
title_short |
Structural characterization of kerogen in 3.4 Ga Archaean |
title_full |
Structural characterization of kerogen in 3.4 Ga Archaean |
title_fullStr |
Structural characterization of kerogen in 3.4 Ga Archaean |
title_full_unstemmed |
Structural characterization of kerogen in 3.4 Ga Archaean |
title_sort |
structural characterization of kerogen in 3.4 ga archaean |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.207.468 http://earthsciences.ucr.edu/docs/Marshall%20et%20al%20%202007%20(2).pdf |
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North Pole |
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North Pole |
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North Pole |
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North Pole |
op_source |
http://earthsciences.ucr.edu/docs/Marshall%20et%20al%20%202007%20(2).pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.207.468 http://earthsciences.ucr.edu/docs/Marshall%20et%20al%20%202007%20(2).pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766140567367974912 |