Fractal analysis of veins in Permian carbonate rocks in the Lingtanchang anticline, western China. Issue 2 (20th August 2013)

• Record Type: Journal Article
• Authors: Deng, B.; Liu, S.; Jansa, L.; Yong, S.; Zhang, Z.
• Is Part Of: Geofluids. Volume 14:Issue 2(2014:May)
• Page Start: 160
• Page End: 173
• Publication Date: 2013-08-20
• Subjects: Hydrogeology -- Periodicals; Sedimentary basins -- Periodicals; Fluids -- Migration -- Periodicals; Groundwater flow -- Periodicals; Geothermal resources -- Periodicals; Fluid dynamics -- Periodicals; Earth -- Crust -- Periodicals; 551.49
• DOI: 10.1111/gfl.12059
• Languages: English
• ISSNs: 1468-8115

Abstract

<abstract abstract-type="main" id="gfl12059-abs-0001"> <title>Abstract</title> <p>Statistical analysis of the thickness distribution of veins in the Lingtanchang structure, southern Sichuan basin, western China, indicates that vein thickness conforms to fractal character and a power‐law distribution, whereas various distributions of veins are indicated by both the spacing distribution and the <italic>C</italic><sub>v</sub> values. According to geometry and structure, the veins in the Lingtanchang structure can be divided into confined and through‐going veins. The statistical analyses show that confined intralayer veins are consistent with a power‐law distribution in thickness, with <italic>D</italic><sub>t</sub> values of 1.1–1.7 and a log‐normal distribution in spacing with <italic>C</italic><sub>v</sub> values of 0.8–0.9. The confined intra‐ to interlayer veins show <italic>D</italic><sub>t</sub> values of 1.0–1.3 and an exponential distribution in spacing, with <italic>C</italic><sub>v</sub> values of 0.9–1.0, indicating an unconnected vein network with weak ability for paleofluid flow. However, the through‐going veins show the lowest <italic>D</italic><sub>t</sub> values of 0.6–0.8 with a power‐law distribution in thickness and power‐law to exponential distribution in spacing with <italic>C</italic><sub>v</sub> values of 1.5–3.2. Differences in spacing distribution and in the thickness of veins can be explained by different stages of vein growth from confined to through‐going veins. Such processes are dominant with percolating cluster models, which significantly controls spatial distribution of veins and paleofluid flow, and therefore the reservoir conditions in the southern Sichuan basin.</p> </abstract>