Oil source and migration process in oblique transfer zone of Fushan Sag, northern South China Sea

Guan-hong Wang , Hua Wang , Hua-jun Gan , Yang Shi , Ying-dong Zhao , Shan-bin Chen

Journal of Central South University ›› 2016, Vol. 23 ›› Issue (3) : 654 -668.

PDF
Journal of Central South University ›› 2016, Vol. 23 ›› Issue (3) : 654 -668. DOI: 10.1007/s11771-016-3111-3
Article

Oil source and migration process in oblique transfer zone of Fushan Sag, northern South China Sea

Author information +
History +
PDF

Abstract

The oblique transfer zone in the Fushan Sag, a syndepositional dome sandwiched between the Bailian and Huangtong sub-sags, has been the most important exploration target. The major oil observation occurs in the E2l1L+M and the E2l3U. 46 oil and rock samples reveal that the oil in the transfer zone is mostly contributed by the Bailian sub-sag, though the source rock conditions, hydrocarbon generation and expulsion histories of the Bailian and Huangtong sub-sags are similar. The E2l3U oil, characterized by high maturity, Pr/Ph ratio and oleanane/C30-hopane ratio, shows a close genetic affinity with the E2l3b source rocks, while the E2l1L+M oil, characterized by lower maturity, Pr/Ph ratio and oleanane/C30-hopane ratio, is suggested to be derived from the E2l1+2b source rocks. The homogenization temperatures of aqueous fluid inclusions, taking the burial history of the reservoirs into account, reflect that the oil charge mainly occurred from mid-Miocene to Pliocene in the oblique transfer zone. The oil transporting passages include connected sand bodies, unconformities and faults in the Fushan Sag. Of these, the faults are the most complicated and significant. The faults differ sharply in the west area, the east area and the oblique transfer zone, resulting in different influence on the oil migration and accumulation. During the main hydrocarbon charge stage, the faults in the west area are characterized by bad vertical sealing and spatially dense distribution. As a result, the oil generated by the Huangtong source rocks is mostly lost along the faults during the vertical migration in the west area. This can be the mechanism proposed to explain the little contribution of the Huangtong source rocks to the oil in the oblique transfer zone. Eventually, an oil migration and accumulation model is built in the oblique transfer zone, which may provide theoretical and practical guides for the oil exploration.

Keywords

oblique transfer zone / oil-source correlation / oil loss / oil migration and accumulation model / Fushan Sag

Cite this article

Download citation ▾
Guan-hong Wang, Hua Wang, Hua-jun Gan, Yang Shi, Ying-dong Zhao, Shan-bin Chen. Oil source and migration process in oblique transfer zone of Fushan Sag, northern South China Sea. Journal of Central South University, 2016, 23(3): 654-668 DOI:10.1007/s11771-016-3111-3

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

DahlstromC. D. A.. Structural geology in the eastern margin of the Canadian rocky mountains [J]. Bulletin of Canadian Petroleum Geology, 1970, 187: 332-406

[2]

ScottD. L., RosendahlB. R.. North Viking Graben: An East African prospective [J]. AAPG Bulletin, 1989, 73(2): 155-165

[3]

MorleyC. K., NelsonR. A., PattonT. L., MunnS. G.. Transfer zones in the East African Rift system and their relevance to hydrocarbon exploration in rifts [J]. AAPG Bulletin, 1990, 74: 1234-1253

[4]

FauldsJ. E., GeissmanJ. W., MawerC. K.. Structural development of a major extensional accommodation zone in the basin and range province, Northwestern Arizona and Southern Navada: Implications for kinematic models of continental extension [C]. Basin and Range Extensional Tectonics Near the Latitude of Las Vegas, Navada. Geological Society of America Memoir, 1990, 176: 37-76

[5]

MoustafaA. R.. Internal structure and deformation of an accommodation zone in the northern part of the Suez rift [J]. Journal of Structural Geology, 1996, 18: 83-108

[6]

FauldsJ. E., VargaR. J.. The role of accommodation zones and transfer zones in the regional segmentation of extended terranes [C]. Accommodation Zones and Transfer Zones: the Regional Segmentation of the Basin and Range Province. Geological Society of American Special Paper, 1998, 323: 1-45

[7]

HouY.-g., HeS., NiJ.-e., WangB.-j.. Tectono-sequence stratigraphic analysis on Paleogene Shahejie Formation in the Banqiao sub-basin, Eastern China [J]. Marine and Petroleum Geology, 2012, 36: 100-117

[8]

SchlischeR. W.. Geometry and origin of fault-related folds in extensional settings [J]. AAPG Bulletin, 1995, 79(11): 1661-1678

[9]

McclayK. R., DooleyT., WhitehouseP., MillsM.. 4-D evolution of rift systems: Insights from scaled physical models [J]. AAPG Bulletin, 2002, 86(6): 935-959

[10]

WangJ.-h., WangH., RenJ.-y., XiaoD.-q., PuX.-g.. A great oblique transition zone in the central Huanghua Sag and its significance for petroleum exploration [J]. Acta Petrolei Sinica, 2010, 31(3): 355-359

[11]

SpechtM., BabyP., OllerJ., MontemuroG., CollettaB., LetouzeyJ., GuillierB.. The boomerang area–An example of oil and gas-fields related to a transfer zone development [J]. AAPG Bulletin, 1993, 77(2): 349-349

[12]

CoskunB.. Oil and gas fields-transfer zone relationships, Thrace basin, NW Turkey [J]. Marine and Petroleum Geology, 1997, 14(4): 401-416

[13]

KornsawanA., MorleyC. K.. The origin and evolution of complex transfer zones (garden shifts) in conjugate fault systems around the Funan Field, Pattani Basin, Gulf of Thailand [J]. Journal of Structural Geology, 2002, 24: 435-449

[14]

LiuE.-t., WangH., LinZ.-l., LiY., MaQ.-l.. Characteristics and hydrocarbon enrichment rules of transfer zone in Fushan Sag, Beibuwan Basin [J]. Journal of Central South University (Science and Technology), 2012, 43: 3946-3953

[15]

LiuE.-t., WangH., LiY., ZhouW., LeonardN. D., LinZ.-l. M. Q.-l.. Sedimentary characteristics and tectonic setting of sublacustrine fans in a half-graben rift depression, Beibuwan Basin, South China Sea [J]. Marine and Petroleum Geology, 2014, 52: 9-21

[16]

LiM.-j., WangT.-g., LiuJ., LuH., WuW.-q., GaoL.-h.. Occurrence and origin of carbon dioxide in the Fushan Depression, Beibuwan Basin, South China Sea [J]. Marine and Petroleum Geology, 2008, 25: 500-513

[17]

LiM.-j., WangT.-g., LiuJ., ZhangM.-z., LuH., MaQ.-l., GaoL.-h.. Biomarker 17a(H)-diahopane: A geochemical tool to study the petroleum system of a Tertiary lacustrine basin, Northern South China Sea [J]. Applied Geochemistry, 2009, 24: 172-183

[18]

ShiX.-b., KohnB., SpencerS., GuoX.-w., LiY.-m., YangX.-q., ShiH.-c., GleadowA.. Cenozoic denudation history of southern Hainan Island, South China Sea: Constrains from low temperature thermochronology [J]. Tectonophysics, 2011, 504(1/2/3/4): 100-115

[19]

MaQ.-l., ZhaoS.-e., LiaoY.-t., LinZ.-l.. Sequence architectures of Paleogene Liushagang Formation and its significance in Fushan sag of the Beibuwan basin [J]. Earth Science–Journal of China University of Geoscience, 2012, 37: 667-678

[20]

LuoQ., PangX.-q.. Reservoir controlling mechanism and petroleum accumulation model for consequent fault and antithetic fault in Fushan Depression of Hainan Area [J]. Acta Petrolei Sinica, 2008, 29: 363-367

[21]

JiangC.-j., LiM.-w., OsadetzK. G., SnowdonL. R., ObermajerM., FowlerM. G.. Bakken/Madison petroleum systems in the Canadian Williston Basin. Part 2: Molecular markers diagnostic of Bakken and Lodgepole source rocks [J]. Organic Geochemistry, 2001, 32: 1037-1054

[22]

TissotB. P., WelteD. H.Petroleum Formation and Occurrence [J], 1984123-147

[23]

MoldowanJ. M., DahlJ., HuizingaB. J., FagoF. J., HickeyL. J., PeakmanT. M., TaylorD. W.. The molecular fossil record of oleanane and its relation to angiosperms [J]. Science, 1994, 265: 768-771

[24]

PeterK. E., WaltersC. C., MoldowanJ. M.The Biomarker Guide [J], 199534-36

[25]

VolkmanJ. K., BarrettS. M., BlackbumS. I.. Eustigmatophyte microalgae are potential sources of C29 sterols, C22-C28 n-alcohols and C28-C32 n-alkyl diols in freshwater environments [J]. Organic Geochemistry, 1999, 30: 307-318

[26]

BaoJ.-p., ZhuC.-s., NiC.-h.. Distribution and composition of biomarkers in crude oils from different sags of Beibuwan Basin [J]. Acta Sedimentologica Sinica, 2007, 25(4): 646-652

[27]

SchoellM., HwangR. J., CarlsonR. M. K., WeltonJ. E.. Carbon isotopic composition of individual biomarkers in gilsonites (Utach) [J]. Organic Geochemistry, 1994, 21: 673-683

[28]

Sinninghe DamstéJ. S., KenigF., KoopmansM. P., KosterJ., SchoutenS., HayesJ. M., DE LeeuwJ. W.. Evidence for gammacerane as an indicator of water column stratification [J]. Geochimica et Cosmochimica Acta, 1995, 59: 1895-1900

[29]

ZhangL.-p., HuangD.-f., LiaoZ.-q.. Gammacerane–Geochemical indicator of water column stratification [J]. Acta Sedimentologica Sinica, 1999, 17(1): 136-140

[30]

MoldowanJ. M., FagoF. J., CarlsonR. M. K., YoungD. C., VAN DuyneG., GlardyJ., SchoellM., PillingerC. T., WattD. S.. Rearranged hopanes in sediments and petroleum [J]. Geochimica et Cosmochimica Acta, 1991, 55: 3333-3353

[31]

LiM.-j., WangT.-g., LiuJ., ZhangM.-z., LuH., MaQ.-l., GaoL.-h.. Oil charging orientation and accumulation characteristics of oil reservoirs in the Fushan Sag, Beibuwan Basin [J]. Petroleum Geology & Experment, 2007, 29(2): 172-177

[32]

MackenzieA. S.Applications of biological markers in petroleum geochemistry [J], 1984115-214

[33]

GranthamP. J.. Steranes isomerization and moretane/hopane ratios in crude oils derived from tertiary source rocks [J]. Organic Geochemistry, 1986, 9: 293-304

[34]

ChenS.-b., GanH.-j., XiaC.-y., ZhaoY.-d., WangG.-h., WangX.. History simulation of thermal evolution and hydrocarbon generation of source rocks in Bailian Sub-sag, Fushan Sag, Beibuwan Basin [J]. Xinjiang Petroleum Geology, 2014, 35(6): 672-677

[35]

ZhangS.-c., LiangD.-g., ZhangB.-m., WangF.-y., BianL.-z., ZhaoM.-j.Generation of marine oil and gas in Tarim basin [J], 2004317-323

[36]

YuJ.-j., LuoQ., ZhangD.-j., LuZ.-h., PangX.-q.. Characteristics of faults in the Fushan Depression of Hainan, Beibuwan Basin and their controlling roles to hydrocarbon pool-formation [J]. Petroleum Geology and Experiment, 2004, 26(3): 241-248

[37]

ChenW., WuZ.-p., HouF., LiW., HouX.-b.. Study on hydrocarbon migration along fault srike [J]. Journal of China University of Petroleum, 2010, 34(6): 25-30

AI Summary AI Mindmap
PDF

106

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/