Thermal maturity oftype II kerogen from the New Albany Shale assessed by 13C CP/MAS NMR

U Werner-Zwanziger; GP Lis; M Mastalerz; A Schimmelmann

doi:10.1016/j.ssnmr.2004.08.001

Thermal maturity oftype II kerogen from the New Albany Shale assessed by 13C CP/MAS NMR

U Werner-Zwanziger, GP Lis, M Mastalerz, A Schimmelmann

Research output: Contribution to journal › Article (Academic Journal) › peer-review

50 Citations (Scopus)

Abstract

Thermal maturity of oil and gas source rocks is typically quantified in terms of vitrinite reflectance, which is based on optical properties of terrestrial woody remains. This study evaluates 13C CP/MAS NMR parameters in kerogen (i.e., the insoluble fraction of organic matter in sediments and sedimentary rocks) as proxies for thermal maturity in marine-derived source rocks where terrestrially derived vitrinite is often absent or sparse. In a suite of samples from the New Albany Shale (Middle Devonian to the Early Mississippian, Illinois Basin) the abundance of aromatic carbon in kerogen determined by 13C CP/MAS NMR correlates linearly well with vitrinite reflectance.

Translated title of the contribution	Thermal maturity oftype II kerogen from the New Albany Shale assessed by 13C CP/MAS NMR
Original language	English
Pages (from-to)	140 - 148
Journal	Solid State Nuclear Magnetic Resonance
Volume	27
DOIs	https://doi.org/10.1016/j.ssnmr.2004.08.001
Publication status	Published - 2005

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10.1016/j.ssnmr.2004.08.001

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title = "Thermal maturity oftype II kerogen from the New Albany Shale assessed by 13C CP/MAS NMR",

abstract = "Thermal maturity of oil and gas source rocks is typically quantified in terms of vitrinite reflectance, which is based on optical properties of terrestrial woody remains. This study evaluates 13C CP/MAS NMR parameters in kerogen (i.e., the insoluble fraction of organic matter in sediments and sedimentary rocks) as proxies for thermal maturity in marine-derived source rocks where terrestrially derived vitrinite is often absent or sparse. In a suite of samples from the New Albany Shale (Middle Devonian to the Early Mississippian, Illinois Basin) the abundance of aromatic carbon in kerogen determined by 13C CP/MAS NMR correlates linearly well with vitrinite reflectance.",

author = "U Werner-Zwanziger and GP Lis and M Mastalerz and A Schimmelmann",

year = "2005",

doi = "10.1016/j.ssnmr.2004.08.001",

language = "English",

volume = "27",

pages = "140 -- 148",

journal = "Solid State Nuclear Magnetic Resonance",

issn = "0926-2040",

publisher = "Elsevier Inc.",

}

TY - JOUR

T1 - Thermal maturity oftype II kerogen from the New Albany Shale assessed by 13C CP/MAS NMR

AU - Werner-Zwanziger, U

AU - Lis, GP

AU - Mastalerz, M

AU - Schimmelmann, A

PY - 2005

Y1 - 2005

N2 - Thermal maturity of oil and gas source rocks is typically quantified in terms of vitrinite reflectance, which is based on optical properties of terrestrial woody remains. This study evaluates 13C CP/MAS NMR parameters in kerogen (i.e., the insoluble fraction of organic matter in sediments and sedimentary rocks) as proxies for thermal maturity in marine-derived source rocks where terrestrially derived vitrinite is often absent or sparse. In a suite of samples from the New Albany Shale (Middle Devonian to the Early Mississippian, Illinois Basin) the abundance of aromatic carbon in kerogen determined by 13C CP/MAS NMR correlates linearly well with vitrinite reflectance.

AB - Thermal maturity of oil and gas source rocks is typically quantified in terms of vitrinite reflectance, which is based on optical properties of terrestrial woody remains. This study evaluates 13C CP/MAS NMR parameters in kerogen (i.e., the insoluble fraction of organic matter in sediments and sedimentary rocks) as proxies for thermal maturity in marine-derived source rocks where terrestrially derived vitrinite is often absent or sparse. In a suite of samples from the New Albany Shale (Middle Devonian to the Early Mississippian, Illinois Basin) the abundance of aromatic carbon in kerogen determined by 13C CP/MAS NMR correlates linearly well with vitrinite reflectance.

U2 - 10.1016/j.ssnmr.2004.08.001

DO - 10.1016/j.ssnmr.2004.08.001

M3 - Article (Academic Journal)

VL - 27

SP - 140

EP - 148

JO - Solid State Nuclear Magnetic Resonance

JF - Solid State Nuclear Magnetic Resonance

SN - 0926-2040

ER -