Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins
Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Liu, Wenhui [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2011 |
|---|
| Anmerkung: |
© Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Chinese journal of geochemistry - SP Science Press, 1985, 30(2011), 1 vom: März, Seite 19-32 |
|---|---|
| Übergeordnetes Werk: |
volume:30 ; year:2011 ; number:1 ; month:03 ; pages:19-32 |
| Links: |
|---|
| DOI / URN: |
10.1007/s11631-011-0483-9 |
|---|
| Katalog-ID: |
OLC2088112022 |
|---|
| LEADER | 01000naa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2088112022 | ||
| 003 | DE-627 | ||
| 005 | 20230303045208.0 | ||
| 007 | tu | ||
| 008 | 230303s2011 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1007/s11631-011-0483-9 |2 doi | |
| 035 | |a (DE-627)OLC2088112022 | ||
| 035 | |a (DE-He213)s11631-011-0483-9-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |a 540 |q VZ |
| 084 | |a 13 |2 ssgn | ||
| 100 | 1 | |a Liu, Wenhui |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins |
| 264 | 1 | |c 2011 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 | ||
| 520 | |a Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. | ||
| 700 | 1 | |a Xu, Yongchang |4 aut | |
| 700 | 1 | |a Tao, Mingxin |4 aut | |
| 700 | 1 | |a Zhang, Xiaobao |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Chinese journal of geochemistry |d SP Science Press, 1985 |g 30(2011), 1 vom: März, Seite 19-32 |w (DE-627)130963208 |w (DE-600)1066729-5 |w (DE-576)077051459 |x 1000-9426 |7 nnns |
| 773 | 1 | 8 | |g volume:30 |g year:2011 |g number:1 |g month:03 |g pages:19-32 |
| 856 | 4 | 1 | |u https://doi.org/10.1007/s11631-011-0483-9 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_2027 | ||
| 951 | |a AR | ||
| 952 | |d 30 |j 2011 |e 1 |c 03 |h 19-32 | ||
| author_variant |
w l wl y x yx m t mt x z xz |
|---|---|
| matchkey_str |
article:10009426:2011----::eimnagnstpgohmsrontrlaeicia |
| hierarchy_sort_str |
2011 |
| publishDate |
2011 |
| allfields |
10.1007/s11631-011-0483-9 doi (DE-627)OLC2088112022 (DE-He213)s11631-011-0483-9-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liu, Wenhui verfasserin aut Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. Xu, Yongchang aut Tao, Mingxin aut Zhang, Xiaobao aut Enthalten in Chinese journal of geochemistry SP Science Press, 1985 30(2011), 1 vom: März, Seite 19-32 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:30 year:2011 number:1 month:03 pages:19-32 https://doi.org/10.1007/s11631-011-0483-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2027 AR 30 2011 1 03 19-32 |
| spelling |
10.1007/s11631-011-0483-9 doi (DE-627)OLC2088112022 (DE-He213)s11631-011-0483-9-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liu, Wenhui verfasserin aut Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. Xu, Yongchang aut Tao, Mingxin aut Zhang, Xiaobao aut Enthalten in Chinese journal of geochemistry SP Science Press, 1985 30(2011), 1 vom: März, Seite 19-32 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:30 year:2011 number:1 month:03 pages:19-32 https://doi.org/10.1007/s11631-011-0483-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2027 AR 30 2011 1 03 19-32 |
| allfields_unstemmed |
10.1007/s11631-011-0483-9 doi (DE-627)OLC2088112022 (DE-He213)s11631-011-0483-9-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liu, Wenhui verfasserin aut Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. Xu, Yongchang aut Tao, Mingxin aut Zhang, Xiaobao aut Enthalten in Chinese journal of geochemistry SP Science Press, 1985 30(2011), 1 vom: März, Seite 19-32 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:30 year:2011 number:1 month:03 pages:19-32 https://doi.org/10.1007/s11631-011-0483-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2027 AR 30 2011 1 03 19-32 |
| allfieldsGer |
10.1007/s11631-011-0483-9 doi (DE-627)OLC2088112022 (DE-He213)s11631-011-0483-9-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liu, Wenhui verfasserin aut Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. Xu, Yongchang aut Tao, Mingxin aut Zhang, Xiaobao aut Enthalten in Chinese journal of geochemistry SP Science Press, 1985 30(2011), 1 vom: März, Seite 19-32 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:30 year:2011 number:1 month:03 pages:19-32 https://doi.org/10.1007/s11631-011-0483-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2027 AR 30 2011 1 03 19-32 |
| allfieldsSound |
10.1007/s11631-011-0483-9 doi (DE-627)OLC2088112022 (DE-He213)s11631-011-0483-9-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liu, Wenhui verfasserin aut Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins 2011 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. Xu, Yongchang aut Tao, Mingxin aut Zhang, Xiaobao aut Enthalten in Chinese journal of geochemistry SP Science Press, 1985 30(2011), 1 vom: März, Seite 19-32 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:30 year:2011 number:1 month:03 pages:19-32 https://doi.org/10.1007/s11631-011-0483-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2027 AR 30 2011 1 03 19-32 |
| language |
English |
| source |
Enthalten in Chinese journal of geochemistry 30(2011), 1 vom: März, Seite 19-32 volume:30 year:2011 number:1 month:03 pages:19-32 |
| sourceStr |
Enthalten in Chinese journal of geochemistry 30(2011), 1 vom: März, Seite 19-32 volume:30 year:2011 number:1 month:03 pages:19-32 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Chinese journal of geochemistry |
| authorswithroles_txt_mv |
Liu, Wenhui @@aut@@ Xu, Yongchang @@aut@@ Tao, Mingxin @@aut@@ Zhang, Xiaobao @@aut@@ |
| publishDateDaySort_date |
2011-03-01T00:00:00Z |
| hierarchy_top_id |
130963208 |
| dewey-sort |
3550 |
| id |
OLC2088112022 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">OLC2088112022</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230303045208.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">230303s2011 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11631-011-0483-9</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2088112022</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11631-011-0483-9-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="a">540</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Liu, Wenhui</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2011</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Yongchang</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tao, Mingxin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Xiaobao</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Chinese journal of geochemistry</subfield><subfield code="d">SP Science Press, 1985</subfield><subfield code="g">30(2011), 1 vom: März, Seite 19-32</subfield><subfield code="w">(DE-627)130963208</subfield><subfield code="w">(DE-600)1066729-5</subfield><subfield code="w">(DE-576)077051459</subfield><subfield code="x">1000-9426</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:30</subfield><subfield code="g">year:2011</subfield><subfield code="g">number:1</subfield><subfield code="g">month:03</subfield><subfield code="g">pages:19-32</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11631-011-0483-9</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">30</subfield><subfield code="j">2011</subfield><subfield code="e">1</subfield><subfield code="c">03</subfield><subfield code="h">19-32</subfield></datafield></record></collection>
|
| author |
Liu, Wenhui |
| spellingShingle |
Liu, Wenhui ddc 550 ssgn 13 Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins |
| authorStr |
Liu, Wenhui |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)130963208 |
| format |
Article |
| dewey-ones |
550 - Earth sciences 540 - Chemistry & allied sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
1000-9426 |
| topic_title |
550 540 VZ 13 ssgn Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins |
| topic |
ddc 550 ssgn 13 |
| topic_unstemmed |
ddc 550 ssgn 13 |
| topic_browse |
ddc 550 ssgn 13 |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Chinese journal of geochemistry |
| hierarchy_parent_id |
130963208 |
| dewey-tens |
550 - Earth sciences & geology 540 - Chemistry |
| hierarchy_top_title |
Chinese journal of geochemistry |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 |
| title |
Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins |
| ctrlnum |
(DE-627)OLC2088112022 (DE-He213)s11631-011-0483-9-p |
| title_full |
Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins |
| author_sort |
Liu, Wenhui |
| journal |
Chinese journal of geochemistry |
| journalStr |
Chinese journal of geochemistry |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2011 |
| contenttype_str_mv |
txt |
| container_start_page |
19 |
| author_browse |
Liu, Wenhui Xu, Yongchang Tao, Mingxin Zhang, Xiaobao |
| container_volume |
30 |
| class |
550 540 VZ 13 ssgn |
| format_se |
Aufsätze |
| author-letter |
Liu, Wenhui |
| doi_str_mv |
10.1007/s11631-011-0483-9 |
| dewey-full |
550 540 |
| title_sort |
helium and argon isotope geochemistry of natural gases in china’s petroliferous basins |
| title_auth |
Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins |
| abstract |
Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. © Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 |
| abstractGer |
Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. © Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 |
| abstract_unstemmed |
Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. © Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2027 |
| container_issue |
1 |
| title_short |
Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins |
| url |
https://doi.org/10.1007/s11631-011-0483-9 |
| remote_bool |
false |
| author2 |
Xu, Yongchang Tao, Mingxin Zhang, Xiaobao |
| author2Str |
Xu, Yongchang Tao, Mingxin Zhang, Xiaobao |
| ppnlink |
130963208 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s11631-011-0483-9 |
| up_date |
2024-07-03T19:37:28.588Z |
| _version_ |
1803587890538610688 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">OLC2088112022</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230303045208.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">230303s2011 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11631-011-0483-9</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2088112022</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11631-011-0483-9-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="a">540</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Liu, Wenhui</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Helium and argon isotope geochemistry of natural gases in China’s petroliferous basins</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2011</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2011</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around $ 10^{−6} $, partly around $ 10^{−7} $. (2) The central stable region: The 3He/4He values are all around $ 10^{−8} $. (3) The western sub-stable region: The 3He/4He values are mainly around $ 10^{−8} $, and around $ 10^{−7} $ on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach $ 10^{−6} $, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some $ CO_{2} $ gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of $ CO_{2} $ and $ CH_{4} $ in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, $ CO_{2} $/3He and $ CH_{4} $/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Yongchang</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tao, Mingxin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Xiaobao</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Chinese journal of geochemistry</subfield><subfield code="d">SP Science Press, 1985</subfield><subfield code="g">30(2011), 1 vom: März, Seite 19-32</subfield><subfield code="w">(DE-627)130963208</subfield><subfield code="w">(DE-600)1066729-5</subfield><subfield code="w">(DE-576)077051459</subfield><subfield code="x">1000-9426</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:30</subfield><subfield code="g">year:2011</subfield><subfield code="g">number:1</subfield><subfield code="g">month:03</subfield><subfield code="g">pages:19-32</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11631-011-0483-9</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">30</subfield><subfield code="j">2011</subfield><subfield code="e">1</subfield><subfield code="c">03</subfield><subfield code="h">19-32</subfield></datafield></record></collection>
|
| score |
7.3984203 |