塔里木盆地现代分支河流体系形态、分布及其主控因素

doi:10.12108/yxyqc.20240405

Lithologic Reservoirs ›› 2024, Vol. 36 ›› Issue (4): 44-56.doi: 10.12108/yxyqc.20240405

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Morphology，distribution and main controlling factors of modern distributive fluvial system in Tarim Basin

MENG Qinghao, ZHANG Changmin, ZHANG Xianghui, ZHU Rui, XIANG Jianbo

School of Geosciences, Yangtze University, Wuhan 430100, China

Received:2023-01-11 Revised:2024-03-24 Online:2024-07-01 Published:2024-07-04

Abstract

Abstract: Combined with the results of field geological investigation，the geographic information software was used to measure the distributive fluvial system（DFS）developed in and around Tarim Basin，and the differences in geometric parameters of DFS in different regions of the basin were compared to study the development rules and main controlling factors of DFS. The results show that：（1）The sedimentary system of Tarim Basin can be divided into four types：DFS，axial sedimentary system，desert sedimentary system and other sedimentary systems. The DFS has the highest proportion，accounting for about 36%，and mainly developed in south Tianshan Mountain piedmont area，the Kunlun Mountain piedmont area and the Altun piedmont area.（2）The DFS in Tarim Basin can be divided into three types：small，large and mega DFS，with the largest scale of DFS deve-loped in the Kunlun Mountain piedmont area，followed by Altun Mountain piedmont area，and the smallest scale in the south Tianshan Mountain piedmont area. Large-scale DFS controls the pattern of DFS. Among the 846 measured DFS， the proportion of small-scale DFS in the basin is 89.4%，and the total area accounts for 5%. The proportion of mega DFS is 2.2%，and the total area accounts for 68%.（3）The main geometric parameters of DFS include area，radius，and slope. The goodness of fit R² between area and radius is 0.966 4，indicating a strong positive correlation. The goodness of fit R² between slope and radius is 0.463 0，indicating a certain degree of negative correlation. The goodness of fit R² between slope and area is 0.498 8，indicating a certain degree of negative correlation.（4）The main controlling factors for the morphology and distribution of DFS include climate，hydrology and tectonic uplift degree. Under extreme arid climate，rivers are more likely to dry up，and the development scale of DFS is limited. The river runoff of DFS has a strong correlation with radius，and the larger the river runoff，the larger the scale of DFS development. The degree of tectonic uplift plays a dominant role，and the higher the mountain uplift，the easier it is to develop larger scale DFS. Negative structural units within the basin promote the development of DFS，while the positive structural units hinder the development of DFS.

Key words: distributive fluvial system, fluvial fan, megafan, geometry, structural uplift degree, negative structural unit, positive structural unit, Quaternary, Tarim Basin, nonmarine basin

CLC Number:

TE121.3

MENG Qinghao, ZHANG Changmin, ZHANG Xianghui, ZHU Rui, XIANG Jianbo. Morphology，distribution and main controlling factors of modern distributive fluvial system in Tarim Basin[J].Lithologic Reservoirs, 2024, 36(4): 44-56.

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Morphology，distribution and main controlling factors of modern distributive fluvial system in Tarim Basin

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