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PSSalt Tectonics and Their Relationships to Hydrocarbons in the Kuqa Foreland Fold-and-Thrust Belt, Northern Tarim Basin, China*
Yixin Yu1 and Liangjie Tang1
Search and Discovery Article #10157 (2009)
Posted February 5, 2009
*Adapted from poster presentation AAPG Convention, San Antonio, TX, April 20-23, 2008
1State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing, China. ([email protected])
The aim of this article is to investigate the styles, evolution, and controlling mechanisms of salt tectonics and their relationships to hydrocarbons in the Kuqa foreland fold-and-thrust belt, northern Tarim basin, northwestern China. The field observations and interpretation of seismic profiles show that the salt tectonics, which can be divided into salt nappes, salt pillows, salt walls, salt welds, mini-basins, and fish-tails of varying scales, are well developed in the Kuqa region. The intense structural
distortion of salt tectonics occurred in the later Himalayan period from the Kuqa period to Quaternary. To comparatively analyze the major factors influencing the development of salt tectonics, the model of elastic-viscous plate showing the relationships between the salt and overburden has been established by virtue of thin film theory. The results indicate that the differential loading induced by the thicker sediments in the Baicheng sag dominated in the early stage of salt flowage. At present, however, the compressional stresses are the most important factor governing the development of salt tectonics. In addition, physical modelling demonstrates that the pre-Paleogene basement tectonics had important influence on the development of salt tectonics. The salt tectonics exerted important influence on the hydrocarbon accumulations in the Kuqa foreland fold-and-thrust belt. The
structural
and subtle traps induced by the salt tectonics offered abundant favorable spaces for hydrocarbon accumulations; the faults acted as favorable pathways for hydrocarbon migration, and the thick halite layers served as good regional seals for hydrocarbon preservation. The models of hydrocarbon accumulations are different in the subsalt, salt, and suprasalt in the Kuqa foreland fold-and-thrust belt.
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Geological Setting
The Kuqa foreland fold-and-thrust belt, covering an area of about 28,000 square kilometers, is located in the north of Tarim basin and is bounded to the north and south by the South Tianshan Mountains Orogen and Tabei Uplift, respectively. The Kuqa fold-and-thrust belt is one of the important
Geometric Features of Salt Tectonics
The Kuqa foreland fold-and-thrust belt is dominated by the complicated salt
Evolution of Salt Tectonics
The balanced
Relationships of Salt Tectonics to Hydrocarbons
Some large fields which have close relationships to salt tectonics have been discovered in the Kuqa foreland fold-and-thrust belt, such as the Kela-2 gas field, Dina-2 gas field, and Dabei gas field (Figure 6). The relationships of salt tectonics to hydrocarbons can be simply summarized as follows: 1) Salt flowage can change the overburden and then produce various
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