Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China

Abstract In this paper, the data of thin section, organic petrology, geochemistry, lithology and porosity were used to investigate enrichment conditions of Hetaoyuan Formation shale oil in the Biyang Depression. The results show the shale oil is a kind of low-maturity oil with medium density and low...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Shang, Fei [verfasserIn] Xie, Xinong Li, Shuifu

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2018

Schlagwörter:	Shale oil Hydrocarbon enrichment condition Overpressure Lacustrine shale Biyang Depression

Anmerkung:	© The Author(s) 2018

Übergeordnetes Werk:	Enthalten in: Journal of petroleum exploration and production technology - Berlin : Springer, 2011, 9(2018), 2 vom: 11. Okt., Seite 927-936
Übergeordnetes Werk:	volume:9 ; year:2018 ; number:2 ; day:11 ; month:10 ; pages:927-936

Links:	Volltext

DOI / URN:	10.1007/s13202-018-0565-x

Katalog-ID:	SPR031508537

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allfields	10.1007/s13202-018-0565-x doi (DE-627)SPR031508537 (SPR)s13202-018-0565-x-e DE-627 ger DE-627 rakwb eng Shang, Fei verfasserin (orcid)0000-0003-4986-3061 aut Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2018 Abstract In this paper, the data of thin section, organic petrology, geochemistry, lithology and porosity were used to investigate enrichment conditions of Hetaoyuan Formation shale oil in the Biyang Depression. The results show the shale oil is a kind of low-maturity oil with medium density and low viscosity, and main factors controlling shale oil enrichment include total organic content (TOC), formation pressure, lithofacies and effective reservoirs. Shales in the fifth organic-rich interval are developed widely with large thickness (reach up to 150 m), high TOC content (2.0–4.68%), better organic matter types (type I and $ II_{1} $) and appropriate thermal maturity (usually larger than 0.5%), which are beneficial to generate much hydrocarbon, and volume expansion causes overpressure in source rock, especially in sections with low hydrocarbon expulsion efficiency due to less fractures. Free hydrocarbons S1 values increase with TOC contents, and significant overpressure correlates with the larger OSI (S1/TOC × 100) values and porosity. Well-developed calcareous shales and argillaceous shales with silty shale interlayers have better porosity, and effective pores (throat diameters greater than 10 nm) contribute to 47.5% of the total volume. Shale oil (dpeaa)DE-He213 Hydrocarbon enrichment condition (dpeaa)DE-He213 Overpressure (dpeaa)DE-He213 Lacustrine shale (dpeaa)DE-He213 Biyang Depression (dpeaa)DE-He213 Xie, Xinong aut Li, Shuifu aut Enthalten in Journal of petroleum exploration and production technology Berlin : Springer, 2011 9(2018), 2 vom: 11. Okt., Seite 927-936 (DE-627)647654148 (DE-600)2595714-4 2190-0566 nnns volume:9 year:2018 number:2 day:11 month:10 pages:927-936 https://dx.doi.org/10.1007/s13202-018-0565-x kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2009 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_2129 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2018 2 11 10 927-936
spelling	10.1007/s13202-018-0565-x doi (DE-627)SPR031508537 (SPR)s13202-018-0565-x-e DE-627 ger DE-627 rakwb eng Shang, Fei verfasserin (orcid)0000-0003-4986-3061 aut Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2018 Abstract In this paper, the data of thin section, organic petrology, geochemistry, lithology and porosity were used to investigate enrichment conditions of Hetaoyuan Formation shale oil in the Biyang Depression. The results show the shale oil is a kind of low-maturity oil with medium density and low viscosity, and main factors controlling shale oil enrichment include total organic content (TOC), formation pressure, lithofacies and effective reservoirs. Shales in the fifth organic-rich interval are developed widely with large thickness (reach up to 150 m), high TOC content (2.0–4.68%), better organic matter types (type I and $ II_{1} $) and appropriate thermal maturity (usually larger than 0.5%), which are beneficial to generate much hydrocarbon, and volume expansion causes overpressure in source rock, especially in sections with low hydrocarbon expulsion efficiency due to less fractures. Free hydrocarbons S1 values increase with TOC contents, and significant overpressure correlates with the larger OSI (S1/TOC × 100) values and porosity. Well-developed calcareous shales and argillaceous shales with silty shale interlayers have better porosity, and effective pores (throat diameters greater than 10 nm) contribute to 47.5% of the total volume. Shale oil (dpeaa)DE-He213 Hydrocarbon enrichment condition (dpeaa)DE-He213 Overpressure (dpeaa)DE-He213 Lacustrine shale (dpeaa)DE-He213 Biyang Depression (dpeaa)DE-He213 Xie, Xinong aut Li, Shuifu aut Enthalten in Journal of petroleum exploration and production technology Berlin : Springer, 2011 9(2018), 2 vom: 11. Okt., Seite 927-936 (DE-627)647654148 (DE-600)2595714-4 2190-0566 nnns volume:9 year:2018 number:2 day:11 month:10 pages:927-936 https://dx.doi.org/10.1007/s13202-018-0565-x kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2009 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_2129 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2018 2 11 10 927-936
allfields_unstemmed	10.1007/s13202-018-0565-x doi (DE-627)SPR031508537 (SPR)s13202-018-0565-x-e DE-627 ger DE-627 rakwb eng Shang, Fei verfasserin (orcid)0000-0003-4986-3061 aut Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2018 Abstract In this paper, the data of thin section, organic petrology, geochemistry, lithology and porosity were used to investigate enrichment conditions of Hetaoyuan Formation shale oil in the Biyang Depression. The results show the shale oil is a kind of low-maturity oil with medium density and low viscosity, and main factors controlling shale oil enrichment include total organic content (TOC), formation pressure, lithofacies and effective reservoirs. Shales in the fifth organic-rich interval are developed widely with large thickness (reach up to 150 m), high TOC content (2.0–4.68%), better organic matter types (type I and $ II_{1} $) and appropriate thermal maturity (usually larger than 0.5%), which are beneficial to generate much hydrocarbon, and volume expansion causes overpressure in source rock, especially in sections with low hydrocarbon expulsion efficiency due to less fractures. Free hydrocarbons S1 values increase with TOC contents, and significant overpressure correlates with the larger OSI (S1/TOC × 100) values and porosity. Well-developed calcareous shales and argillaceous shales with silty shale interlayers have better porosity, and effective pores (throat diameters greater than 10 nm) contribute to 47.5% of the total volume. Shale oil (dpeaa)DE-He213 Hydrocarbon enrichment condition (dpeaa)DE-He213 Overpressure (dpeaa)DE-He213 Lacustrine shale (dpeaa)DE-He213 Biyang Depression (dpeaa)DE-He213 Xie, Xinong aut Li, Shuifu aut Enthalten in Journal of petroleum exploration and production technology Berlin : Springer, 2011 9(2018), 2 vom: 11. Okt., Seite 927-936 (DE-627)647654148 (DE-600)2595714-4 2190-0566 nnns volume:9 year:2018 number:2 day:11 month:10 pages:927-936 https://dx.doi.org/10.1007/s13202-018-0565-x kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2009 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_2129 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2018 2 11 10 927-936
allfieldsGer	10.1007/s13202-018-0565-x doi (DE-627)SPR031508537 (SPR)s13202-018-0565-x-e DE-627 ger DE-627 rakwb eng Shang, Fei verfasserin (orcid)0000-0003-4986-3061 aut Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2018 Abstract In this paper, the data of thin section, organic petrology, geochemistry, lithology and porosity were used to investigate enrichment conditions of Hetaoyuan Formation shale oil in the Biyang Depression. The results show the shale oil is a kind of low-maturity oil with medium density and low viscosity, and main factors controlling shale oil enrichment include total organic content (TOC), formation pressure, lithofacies and effective reservoirs. Shales in the fifth organic-rich interval are developed widely with large thickness (reach up to 150 m), high TOC content (2.0–4.68%), better organic matter types (type I and $ II_{1} $) and appropriate thermal maturity (usually larger than 0.5%), which are beneficial to generate much hydrocarbon, and volume expansion causes overpressure in source rock, especially in sections with low hydrocarbon expulsion efficiency due to less fractures. Free hydrocarbons S1 values increase with TOC contents, and significant overpressure correlates with the larger OSI (S1/TOC × 100) values and porosity. Well-developed calcareous shales and argillaceous shales with silty shale interlayers have better porosity, and effective pores (throat diameters greater than 10 nm) contribute to 47.5% of the total volume. Shale oil (dpeaa)DE-He213 Hydrocarbon enrichment condition (dpeaa)DE-He213 Overpressure (dpeaa)DE-He213 Lacustrine shale (dpeaa)DE-He213 Biyang Depression (dpeaa)DE-He213 Xie, Xinong aut Li, Shuifu aut Enthalten in Journal of petroleum exploration and production technology Berlin : Springer, 2011 9(2018), 2 vom: 11. Okt., Seite 927-936 (DE-627)647654148 (DE-600)2595714-4 2190-0566 nnns volume:9 year:2018 number:2 day:11 month:10 pages:927-936 https://dx.doi.org/10.1007/s13202-018-0565-x kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2009 GBV_ILN_2014 GBV_ILN_2027 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_2129 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2018 2 11 10 927-936
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topic_facet	Shale oil Hydrocarbon enrichment condition Overpressure Lacustrine shale Biyang Depression
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author	Shang, Fei
spellingShingle	Shang, Fei misc Shale oil misc Hydrocarbon enrichment condition misc Overpressure misc Lacustrine shale misc Biyang Depression Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China
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topic_title	Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China Shale oil (dpeaa)DE-He213 Hydrocarbon enrichment condition (dpeaa)DE-He213 Overpressure (dpeaa)DE-He213 Lacustrine shale (dpeaa)DE-He213 Biyang Depression (dpeaa)DE-He213
topic	misc Shale oil misc Hydrocarbon enrichment condition misc Overpressure misc Lacustrine shale misc Biyang Depression
topic_unstemmed	misc Shale oil misc Hydrocarbon enrichment condition misc Overpressure misc Lacustrine shale misc Biyang Depression
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title	Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China
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title_full	Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China
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title_sort	enrichment conditions of hetaoyuan formation shale oil in biyang depression, china
title_auth	Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China
abstract	Abstract In this paper, the data of thin section, organic petrology, geochemistry, lithology and porosity were used to investigate enrichment conditions of Hetaoyuan Formation shale oil in the Biyang Depression. The results show the shale oil is a kind of low-maturity oil with medium density and low viscosity, and main factors controlling shale oil enrichment include total organic content (TOC), formation pressure, lithofacies and effective reservoirs. Shales in the fifth organic-rich interval are developed widely with large thickness (reach up to 150 m), high TOC content (2.0–4.68%), better organic matter types (type I and $ II_{1} $) and appropriate thermal maturity (usually larger than 0.5%), which are beneficial to generate much hydrocarbon, and volume expansion causes overpressure in source rock, especially in sections with low hydrocarbon expulsion efficiency due to less fractures. Free hydrocarbons S1 values increase with TOC contents, and significant overpressure correlates with the larger OSI (S1/TOC × 100) values and porosity. Well-developed calcareous shales and argillaceous shales with silty shale interlayers have better porosity, and effective pores (throat diameters greater than 10 nm) contribute to 47.5% of the total volume. © The Author(s) 2018
abstractGer	Abstract In this paper, the data of thin section, organic petrology, geochemistry, lithology and porosity were used to investigate enrichment conditions of Hetaoyuan Formation shale oil in the Biyang Depression. The results show the shale oil is a kind of low-maturity oil with medium density and low viscosity, and main factors controlling shale oil enrichment include total organic content (TOC), formation pressure, lithofacies and effective reservoirs. Shales in the fifth organic-rich interval are developed widely with large thickness (reach up to 150 m), high TOC content (2.0–4.68%), better organic matter types (type I and $ II_{1} $) and appropriate thermal maturity (usually larger than 0.5%), which are beneficial to generate much hydrocarbon, and volume expansion causes overpressure in source rock, especially in sections with low hydrocarbon expulsion efficiency due to less fractures. Free hydrocarbons S1 values increase with TOC contents, and significant overpressure correlates with the larger OSI (S1/TOC × 100) values and porosity. Well-developed calcareous shales and argillaceous shales with silty shale interlayers have better porosity, and effective pores (throat diameters greater than 10 nm) contribute to 47.5% of the total volume. © The Author(s) 2018
abstract_unstemmed	Abstract In this paper, the data of thin section, organic petrology, geochemistry, lithology and porosity were used to investigate enrichment conditions of Hetaoyuan Formation shale oil in the Biyang Depression. The results show the shale oil is a kind of low-maturity oil with medium density and low viscosity, and main factors controlling shale oil enrichment include total organic content (TOC), formation pressure, lithofacies and effective reservoirs. Shales in the fifth organic-rich interval are developed widely with large thickness (reach up to 150 m), high TOC content (2.0–4.68%), better organic matter types (type I and $ II_{1} $) and appropriate thermal maturity (usually larger than 0.5%), which are beneficial to generate much hydrocarbon, and volume expansion causes overpressure in source rock, especially in sections with low hydrocarbon expulsion efficiency due to less fractures. Free hydrocarbons S1 values increase with TOC contents, and significant overpressure correlates with the larger OSI (S1/TOC × 100) values and porosity. Well-developed calcareous shales and argillaceous shales with silty shale interlayers have better porosity, and effective pores (throat diameters greater than 10 nm) contribute to 47.5% of the total volume. © The Author(s) 2018
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title_short	Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China
url	https://dx.doi.org/10.1007/s13202-018-0565-x
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Enrichment conditions of Hetaoyuan Formation shale oil in Biyang Depression, China

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