Publicado

2019-04-01

Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China

Estructuras de deformación de sedimentos blandos y arquitectura de cuerpos de arena en el miembro de petróleo Chang 6 de la formación Yanchang del Triásico Superior, al suroeste de la cuenca Ordos de China

DOI:

https://doi.org/10.15446/esrj.v23n2.72414

Palabras clave:

soft-sediment deformation structure, sand body architecture, Chang6 oil member, Yanchang Formation, Ordos Basin, (en)
Estructuras de deformación de sedimentos blandos, arquitectura de sedimentos blandos, miembro petrolífero Chang 6, Formación Yanchang, Cuenca Ordos, (es)

Descargas

Autores/as

  • Qingshao Liang Chengdu University of Technology
  • Jingchun Tian Chengdu University of Technology
  • Feng Wang Chengdu University of Technology
  • Xiang Zhang Chengdu University of Technology
Soft-sediment deformation (SSD) structures of the Upper Triassic Yanchang Formation are laterally widespread in the Ordos Basin. In the Huachi-Qingyang (H-Q) area of the Ordos Basin, the Chang6 oil member of the Upper Triassic Yanchang Formation is among the most significant Mesozoic oil-bearing strata. It is characterized by the development of reservoir sand bodies. During the depositional evolution of the Chang6 oil member, SSD structures induced by paleo-seismic events developed in the H-Q area in the middle of the basin. The SSD structures developed in the sand bodies of the Chang6 oil member are mainly ball-and-pillow structures, fold structures, sand dikes, irregular convolute stratifications and synsedimentary faults. The architecture of the sand bodies resulted from paleo-seismic events and gravity slumping and mainly include two types of structures: 1) SSD structures driven by paleo-seismic events with normal sedimentation (delta front sand body) (SN-SSD) and 2) SSD structures driven by paleo-seismic events with turbidites (formed by delta-front slumping and re-distribution due to seismic action) (ST-SSD). As a consequence, genetic models of the sand bodies formed by different sedimentation processes are established.

Las estructuras de deformación de sedimentos blandos de la Formación Yanchang del Triásico Superior están extendidas lateralmente en la cuenca Ordos. En el área Huachi-Qingyang de esta cuenca, el miembro de petróleo Chang 6 está entre los estratos petrolíferos más significativos del Mesozoico. Este se caracteriza por el desarrollo de cuerpos de arena en el yacimiento. Durante la evolución deposicional del miembro Chang 6, las estructuras de deformación de sedimentos blandos se desarrollaron en el área Huachi-Qingyang, en el medio de la cuenca, inducidas por eventos paleosísmicos. Las estructuras de deformación de sedimentos blandos que se desarrollaron en los cuerpos de arenas del miembro de petróleo Chang 6 son principalmente estructuras esféricas y acojinadas, estructuras plegadas, canales de arena, estratificaciones irregulares enrolladas y fallas sinsedimentarias. La arquitectura de los cuerpos arenosos son el resultado de eventos paleosísmicos y la caída por gravedad; se reconocen principalmente dos tipos de estructuras: 1. Estructuras de deformación de sedimentos blandos por eventos paleosísmicos con cuerpos arenosos del frente del delta. 2. Estructuras de deformación de sedimentos blandos traídas por eventos paleosísmicos con turbiditas (formadas por la caída del frente del delta y redistribuidas debido a la acción sísmica). Como consecuencia, se establecieron los modelos genéticos de los cuerpos arenosos formados por diferentes procesos de sedimentación.

Referencias

Alfaro, P., Delgado, J., Estévez, A., Molina, J. M., Moretti, M. & Soria, J. M. (2002). Liquefaction and fluidization structures in Messinian storm deposits (Bajo Segura Basin, Betic Cordillera, southern Spain). International Journal of Earth Sciences, 91, 505–513.

Allen, J. R. L. (1982). Sedimentary structures: their character and physical basis. Elsevier, Amsterdam. Vol. II, 663p.

Bachmann, G. H. & Aref, M. A. M. (2005). A seismite in Triassic gypsum deposits (Grabfeld Formation, Ladinian), southwestern Germany. Sedimentary Geology, 180, 75–89.

Becker, A., Davenport, C. A. & Giardini, D. (2002). Palaeoseismicity studies on end-Pleistocene and Holocene lake deposits around Basle, Switzerland. Geophysical Journal International, 149, 659–678.

Brands, C. & Winsemann, J. (2013). Soft-sediment deformation structures in Late Pleistocene alluvial-aeolian sediments caused by GIA induced seismicity along the Osning Thrust (northern Germany). In : EGU General Assembly 2013, held 7-12 April, 2013 in Vienna, Austria, id. EGU2013-2844.

Calvo, J. P., Rodríguez-Pascua, M. A., Martín-Velázquez, S., Jimenez, S. & De Vicente, G. (1998). Microdeformation of lacustrine laminite sequences from Late Miocene formations of SE Spain: an interpretation of loop bedding. Sedimentology, 45, 279-292.

Gao, L.X., Hou, D., Li, J., Li, S.H., Dai, Y., Xiong, F. & Yang, H.Y. (2016). Movement characteristics and present seismic activity of Ordos Block. Geodesy and Geodynamics 7 (6), 451-458.

Ghosh, S. K., Singh, S. S., Ray, Y. & Sinha, S. (2010). Soft-sedimentary deformational structures: seismites or penecontemporaneous, a study from the Palaeoproterozoic Lesser Himalayan succession. Current Science, 98, 247–253.

Li, J., Chen, H. D., Lin, L. B., Zhao, J. X., Chen, A. Q., Zhu, Z. J., Peng, C. L., Zhang, C. G. & Chen, Y. Q. (2010). Effect of ancient earthquake and its geological significance of Upper Triassic Yanchang Formation in Southeast Ordos Basin (in Chinese with English abstract). Geological Review, 56 (4), 480-489.

Li, W. H., Pang, J. G., Cao, H. X., Xiao, L. & Wang, R. G. (2009). Depositional system and paleogeographic evolution of the Late Triassic Yanchang Stage in Ordos Basin (in Chinese with English abstract). Journal of Northwest University (Natural Science Edition), 39 (3), 501-506.

Liu, L., Zhong, Y., Chen, H., Xu, C. & Wu, K. (2016). Seismically induced soft-sediment deformation structures in the palaeogene deposits of the Liaodong bay depression in the Bohai bay basin and their spatial stratigraphic distribution. Sedimentary Geology, 342, 78-90.

Martín-Chivelet, J., Palma, R. M., López-Gómez, J. & Kietzmann, D. A. (2011). Earthquake induced soft-sediment deformation structures in Upper Jurassic open-marine microbialites (Neuquén Basin, Argentina). Sedimentary Geology, 235, 210–221.

Montenat, C., Barrier, P., Philippe Ott d’Estevou & Hibsch, C. (2007). Seismites: An attempt at critical analysis and classification. Sedimentary Geology, 196(1), 5-30.

Moretti, M. & Sabato, L. (2007). Recognition of trigger mechanisms for soft-sediment deformation in the Pleistocene lacustrine deposits of the Sant'Arcangelo Basin (southern Italy): seismic shock vs. overloading. Sedimentary Geology, 196, 31–45.

Moretti, M. & Ronchi, A. (2011). Liquefaction features interpreted as seismites in the Pleistocene fluvio-lacustrine deposits of the Neuquen Basin (NorthernPatagonia). Sedimentary Geology, 235, 200–209.

Obermeier, S.F. (2009). Using liquefaction-induced and other soft-sediment features for paleoseismic analysis. International Geophysics, 95, 497-564.

Owen, G. (1987). Deformation processes in unconsolidated sands. In: Jones, M. E., Preston, R. M. F. (Eds.), Deformation of sediments and sedimentary rocks: Geological Society Special Publication, 29, pp. 11–24.

Owen, G. & Moretti, M. (2011). Identifying triggers for liquefaction-induced soft-sediment deformation in sands. Sedimentary Geology, 235, 141–147.

Oliveira, C. M. M., Hodgson, D. M. & Flint, S. (2011). Distribution of soft-sediment deformation structures in clinoform successions of the Permian Ecca Group, Karoo Basin, South Africa. Sedimentary Geology, 235, 314–330.

Onorato, M. R., Perucca, L., Coronato, A., Rabassa, J. & Lopez, R. (2016). Seismically-induced soft-sediment deformation structures associated with the Magallanes-Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina). Sedimentary Geology, 344, 135-144.

Pang, J. G., Guo, J. A., Song, L. J. & Li, W. H. (2012). The event deposits from the Yangchangian lacustrine basin in the Ordos Basin (in Chinese with English abstract). Sedimentary Geology and Tethyan Geology, 32(1), 32-37.

Papadopoulos, G. A. & Lefkopoulos, G. (1993). Magnitude-distance relations for liquefaction in soil from earthquakes. Bulletin of the Seismological Society of America, 83(3), 925-938.

Qiao, X., Song, T., Gao, L., Peng, Y. & Li, H. (1994). Seismic sequence in carbonate rocks by vibrational liquefaction (in Chinese with English abstract). Acta Geologica Sinica, 68(1), 16-36.

Qiu, X., Liu, C., Mao, G., Deng, Y., Wang, F. & Wang, J. (2014). Late Triassic tuff intervals in the Ordos basin, Central China: Their depositional, petrographic, geochemical characteristics and regional implications. Journal of Asian Earth Sciences 80, 148-160.

Qiu, X., Liu, C., Wang, F., Deng, Y. & Mao, G. (2015). Trace and rare earth element geochemistry of the Upper Triassic mudstones in the southern Ordos Basin, Central China. Geological Journal, 50, 399-413.

Rodríguez-Pascua, M. A., Calvo, J. P., De Vicente, G. & Gómez-Gras, D. (2000). Soft-sediment deformation structures interpreted as seismites in lacustrine sediments of the Prebetic Zone, SE Spain, and their potential use as indicators of earthquake magnitudes during the Late Miocene. Sedimentary Geology, 135, 117–135.

Scott, B. & Price, S. (1988). Earthquake-induced structures in young sediments. Tectonophysics, 147, 165–170.

Seilacher, A. (1969). Fault-grade bed interpreted as seismites. Sedimentology, 13, 155–159.

Seilacher, A. (1984). Sedimentary structures tentatively attributed to seismic events. Marine Geology, 55, 1–12.

Sims, J. D. (1975). Determining earthquake recurrence intervals from deformational structures in young lacustrine sediments. Tectonophysics, 29, 141–152.

Tian, Y., Zhong, J. H., Wang, S. B. & Tao, H. S. (2015). Seismites and their geological significances of the Triassic Yanchang Formation in Fuxian exploration area, Ordos Basin (in Chinese with English abstract). Journal of Palaeogeography, 17(4), 541-552.

Tuttle, M. P. & Schweig, E. S. (1996) Recognizing and dating prehistoric liquefaction features: Lessons learned in the New Madrid seismic zone, central United States. Journal of Geophysical Research, 101, 6171-6178.

Van Loon, A. J. & Pisarska-Jamrozy, M. (2014). Sedimentological evidence of Pleistocene earthquakes in NW Poland induced by glacio-isostatic rebound. Sedimentary Geology, 300, 1–10.

Xia, Q. S., Tian, J. C. & Huang, C. W. (2007). Study on the recognition marks of seiemites in Upper Triassic Yanchang Formation, Ordos Basin, China (in Chinese with English abstract). Journal of Chengdu University of Technology (Science & Technology Edition), 34(03), 312-317.

Yan, J. H., Cui, Y. B. & Chen, S. Y. (2009). Identification of common facies indicators of seismites in simulated experiments (in Chinese with English abstract). Acta Sedimentology Sinica, 27(6), 1131-1137.

Yang, R. C., Van Loon, A. J., Yin, W., Fan, A. P. & Han, Z. Z. (2016). Soft-sediment deformation structures in cores from lacustrine slurry deposits of the Late Triassic Yanchang Fm. (central China). Geologos, 22(3), 201-211.

Yang, R. C., Fan, A. P., Han, Z. Z. & Van Loon, A. J. (2017). Lithofacies and origin of the Late Trissic muddy gravity-flow deposits in the Ordos Basin, central China. Marine and Petroleum Geology, 85, 194-219.

Zhang, C., Wu, Z., Gao, L., Wang, W., Tian, Y. & Ma, C. (2007). Earthquake-induced soft sediment deformation structures in the Mesopro-terozoic Wumishan Formation, North China, and their geologic implications. Science in China Series D: Earth Sciences, 50, 350–358.

Zhang, Y. Q., Mercier, J. L. & Vergely, P. (1998). Extension in the graben systems around the Ordos (China), and its contribution to the extrusion tectonics of south China with respect to Gobi-Mongolia. Tectonophysics, 285, 41-75.

Zheng, R. C., Wang, C. Y., Wang, H. H, Wang, C. Y. & Wen, H. G. (2009). Sequence-based lithofacies and paleogeographic characteristics of 6th oil-bearing member of the Yanchang Formation of Upper Triassic in the Shijiawan area, Ordos Basin (in Chinese with English abstract). Journal of Mineralogy and Petrology, 29(4), 16-24.

Cómo citar

APA

Liang, Q., Tian, J., Wang, F. y Zhang, X. (2019). Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China. Earth Sciences Research Journal, 23(2), 119–126. https://doi.org/10.15446/esrj.v23n2.72414

ACM

[1]
Liang, Q., Tian, J., Wang, F. y Zhang, X. 2019. Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China. Earth Sciences Research Journal. 23, 2 (abr. 2019), 119–126. DOI:https://doi.org/10.15446/esrj.v23n2.72414.

ACS

(1)
Liang, Q.; Tian, J.; Wang, F.; Zhang, X. Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China. Earth sci. res. j. 2019, 23, 119-126.

ABNT

LIANG, Q.; TIAN, J.; WANG, F.; ZHANG, X. Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China. Earth Sciences Research Journal, [S. l.], v. 23, n. 2, p. 119–126, 2019. DOI: 10.15446/esrj.v23n2.72414. Disponível em: https://revistas.unal.edu.co/index.php/esrj/article/view/72414. Acesso em: 19 jul. 2024.

Chicago

Liang, Qingshao, Jingchun Tian, Feng Wang, y Xiang Zhang. 2019. «Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China». Earth Sciences Research Journal 23 (2):119-26. https://doi.org/10.15446/esrj.v23n2.72414.

Harvard

Liang, Q., Tian, J., Wang, F. y Zhang, X. (2019) «Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China», Earth Sciences Research Journal, 23(2), pp. 119–126. doi: 10.15446/esrj.v23n2.72414.

IEEE

[1]
Q. Liang, J. Tian, F. Wang, y X. Zhang, «Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China», Earth sci. res. j., vol. 23, n.º 2, pp. 119–126, abr. 2019.

MLA

Liang, Q., J. Tian, F. Wang, y X. Zhang. «Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China». Earth Sciences Research Journal, vol. 23, n.º 2, abril de 2019, pp. 119-26, doi:10.15446/esrj.v23n2.72414.

Turabian

Liang, Qingshao, Jingchun Tian, Feng Wang, y Xiang Zhang. «Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China». Earth Sciences Research Journal 23, no. 2 (abril 1, 2019): 119–126. Accedido julio 19, 2024. https://revistas.unal.edu.co/index.php/esrj/article/view/72414.

Vancouver

1.
Liang Q, Tian J, Wang F, Zhang X. Soft-sediment Deformation Structures and Sand Body Architecture in the Chang 6 Oil Member of the Upper Triassic Yanchang Formation, Southwestern Ordos Basin, China. Earth sci. res. j. [Internet]. 1 de abril de 2019 [citado 19 de julio de 2024];23(2):119-26. Disponible en: https://revistas.unal.edu.co/index.php/esrj/article/view/72414

Descargar cita

CrossRef Cited-by

CrossRef citations5

1. Márcio Lima Alencar, Osvaldo José Correia Filho, Tiago Siqueira de Miranda, José Antonio Barbosa, Maria Alcione Lima Celestino, Germano Mário Silva Ramos, Araly Fabiana Lima de Araújo, Virginio Henrique Neumann, João Gabriel de Oliveira Topan, Eduardo Roemers-Oliveira. (2021). Soft-sediment deformation structures in Aptian lacustrine laminites: Evidence of post-rift paleoseismicity in the Araripe basin, NE Brazil. Journal of South American Earth Sciences, 105, p.102955. https://doi.org/10.1016/j.jsames.2020.102955.

2. Pengpeng Fan, Rui Deng, Jinquan Qiu, Zhongliang Zhao, Shengli Wu. (2021). Well logging curve reconstruction based on kernel ridge regression. Arabian Journal of Geosciences, 14(16) https://doi.org/10.1007/s12517-021-07792-y.

3. Jingchun Tian, Qingshao Liang, Feng Wang, Jian Li, Wei Yu, Weizhen Chen. (2022). Sedimentary records of seismic events in a lacustrine basin of continental depression: A case study of the Triassic Yanchang Formation in the Ordos Basin, Northern China. Journal of Asian Earth Sciences, 228, p.105128. https://doi.org/10.1016/j.jseaes.2022.105128.

4. Wei Yu, Qingshao Liang, Jingchun Tian, Yonglin Han, Feng Wang, Ming Zhao. (2022). Sedimentary Responses of Late Triassic Soft-Sedimentary Deformation to Paleoearthquake Events in the Southwestern North China Plate. Minerals, 12(8), p.1044. https://doi.org/10.3390/min12081044.

5. Walaa A. Hassan, Ezzat A. Ahmed, Rashad Sawires, Mohamed A. Moneim, Mostafa R. Abukhadra. (2022). Evidence for Upper Cretaceous seismites in the Abu Tartur area, Western Desert, Egypt. Journal of African Earth Sciences, 187, p.104452. https://doi.org/10.1016/j.jafrearsci.2022.104452.

Dimensions

PlumX

Visitas a la página del resumen del artículo

481

Descargas

Los datos de descargas todavía no están disponibles.