Sedimentary System and Sand Bodies Distribution of the 2nd Member of Xujiahe Formation in Xinchang Area, Western Sichuan Depression, China

2021 ◽  
pp. 1-54
Author(s):  
Xiaofei Shang ◽  
Meng Li ◽  
Taizhong Duan

The Xujiahe Formation of Late Triassic in the Western Sichuan Depression contains abundant gas reservoirs. Influenced by the thrust tectonic movement of foreland basin, the fluvial-delta sedimentary system supplied by multiple provenances formed the Xu2 Formation of the Xinchang area. We used detailed description of drilling wells and cores to define the sequence stratigraphic framework and sand body types. We used stratal slices through the seismic volume to map the evolution of the sedimentary system and the sand body distribution. The results show that the Xu2 Formation exhibits a complete long-term base-level cycle, and there are six sand body deposit types: distributary channel, inter-channel, subaqueous distributary channel, inter-distributary bay, mouth bar and sheet sand. Stratal slices through the seismic volume at different levels map the spatial variation of sand and mudstone, which we use to construct a sedimentary filling evolution model. This model indicates that during the time of deposition of the Lower Sub-member the main provenance supply came from the NW direction, resulting in the sand bodies mainly deposited in the west. During the time of depositon of the Central Sub-member, sediment supply was large and came from both the NW and NE directions, resulting in large, laterally extensive, thick sands. During the time of deposition of the Upper Sub-member, sediment supply was from the NE direction, with the sand bodies more developed in the east. The flow direction of the channels indicate that they migrated from northwest to northeast. There are differences in channel energy, sedimentary characteristics and reservoir physical properties in the three Sub-members, which cause differences in natural gas productivity of Xu2 Formation. We believe that detailed mapping the spatial distribution of sedimentary systems can provide critical guidance to not only explore, but also to develop in high-quality oil and gas reservoirs like Xu2 Foramtion.

2020 ◽  
Author(s):  
Wenya Lyu ◽  
Lianbo Zeng ◽  
Shuangquan Chen ◽  
Lei Tang ◽  
Yunzhao Zhang

<p>Based on cores, image logs and thin sections, five sets of fractures are developed in the study area, where faults are developed. Most of fractures are open without fillings, and some fractures are filled with calcite, quartz, bitumen, pyrite and mud. Fractures are mainly controlled by lithology, mechanical stratigraphy and faults. Based on mutual crosscutting relationships of fractures, mineral filling sequence of fracture fillings, fluid inclusion and carbon-oxygen isotope analysis of calcite fillings in fractures, and quartz spintronic resonance analysis of quartz fillings in fractures, in combination with thermal and burial history, the formation sequence and time of fractures were analyzed. The results show that fractures mainly formed over three period, that is, the late Triassic, Middle to Late Jurassic, and Late Cretaceous to Paleogene. Then,combined with the paleostress evolution and fracture characteristics of the study area, the formation mechanism of fractures was discussed.</p>


2011 ◽  
Vol 51 (2) ◽  
pp. 713
Author(s):  
Jon Minken ◽  
Phil Cox ◽  
Sandy Buchanan ◽  
Dean Griffin ◽  
Yohan Kusumanegara ◽  
...  

Permit WA-390-P, in Australia’s Exmouth Plateau, has been the subject of an extensive exploration drilling campaign with gas discovered in the Late Triassic Mungaroo Formation and the Cretaceous Lower Barrow Group. Characterisation of these reservoirs with 3D seismic data, well logs, core and biostratigraphic information has allowed insight and refinement to the previously established depositional models. The Mungaroo Formation comprises a thick succession (more than 2 km) of delta plain deposits characterised on 3D seismic by channel morphologies of differing sizes and orientations. Well penetrations in the channels reveal sand-bodies that can be classified as either single-storey or multistorey. Single-storey sand-bodies are thin (less than 15 metres), narrow in planform (less than one kilometer), lack evidence of lateral accretion and occasionally exhibit a funnel geometry. Multistorey channels are characterised by relatively thick, vertically and laterally amalgamated sand-bodies (more than 15 metres), in a broad channel morphology (more than one kilometer) bounded at its base by a composite surface of erosion. Single-storey channels have been interpreted as distributary channels and multistorey channels as incised valleys. In contrast, the Lower Barrow Group is a contemporaneous wave-dominated delta and slope-to-basin-floor sediment gravity flow system. The depositional environments formed progradational clinoform seismic stratigraphic units that filled accommodation generated during rifting. The delta is organised into arcuate to cuspate lobes that show changes in the shelf-slope trajectory with variations in accommodation and sediment supply. During falling trajectories of the shelf-slope break, the slope is demarcated by gullies forming a line of feeder systems that transport sediment from the delta shoreface into the deep-water. The sediment gravity flows formed coalescing fans that blanket the toe-of-slope and basin floor.


2014 ◽  
Vol 608-609 ◽  
pp. 1071-1078
Author(s):  
An Ran Liu ◽  
Xiao Bin Wu ◽  
Jun Ren Hu

Guided by the high-resolution sequence stratigraphy theories, the authors divided the Upper Jurassic Penglaizhen Formation in the middle section of western Sichuan depression of china into 2 long-term sequences (L1-L2) and 4 medium-term sequences (M1-M4) through comprehensive study of outcrops, coring, logging and seismic data. Sequence-based lithofacies and paleogeographic maps of Upper Jurassic Penglaizhen Formation were compiled by medium-term sequences as mapping units. The results showed that the front edge of Longmenshan developed with large-scale alluvial fans, fan delta sediment was a fan-delta group overlapped by several fan deltas at front edge of Longmenshan in period M1-M4.The dominated type of sedimentary system in middle section of western Sichuan depression was fan delta - shallow lake sediment in period M1-M2, alluvial fan was only changed in size and location; sand bodies were mainly distributed in front edge of Longmenshan and the Zhongjiang-Deyang region; In period M3-M4, it is changed into a large area of fan delta plain sediment with thick sand and big scale, sand bodies were mainly distributed in the Pixian-Wenjiang-Dayi area.


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