Helium resource evaluation and enrichment model in Yakela area, Tarim Basin
Received date: 2023-04-27
Revised date: 2023-08-18
Online published: 2023-11-24
Supported by
The National Natural Science Foundation of China(42141021)
the China National Petroleum Corporation-Peking University Strategic Cooperation Basic Research Program “Hydrocarbon accumulation Rule under tectonic-volcanic thermal Event in Tatong area”
A good prospect of helium resources have been found in Yakela area in the north of Tarim Basin. The previous research data have shown that the average content of helium in Paleozoic is 0.31%, which is the stratum with the most abundant helium resources and is higher than the industrial production standard of helium, but the potential of helium resources generation and the reservoir enrichment model in this stratum are still unclear. Based on the natural gamma spectrum logging data of 14 wells in the Yakela area, the helium resource generation of the Paleozoic in the Yakela area was quantitatively evaluated, and combined with the comprehensive analysis of the accumulation factors, the helium enrichment model was summarized according to the helium migration, accumulation processes and carrier characteristics. The results indicate that the average helium generation rate of the Paleozoic in Yakela area is 2.37×10-10 cm3/g and the helium generation is 3.22×109 m3. The area with the highest helium generation rate is predicted to be located near Well Sha 15, followed by the area near Well Sha 49. The main helium generation area is the strip stretching from Well Sha 5 to Well Sha 49. The amount of helium supplied by the Paleozoic sedimentary rock series to the helium-bearing reservoir in the region is higher than the total amount of helium in the natural gas reservoir, and the effective helium source rock can be the sedimentary rock series. With the faults and fractures mainly formed in the Caledonian-Hercynian tectonic period as the migration channels, helium continues to migrate with the help of groundwater and natural gas, and the helium is transported and accumulated by two models, including helium enrichment by ancient formation water moving upward along the fault and helium enrichment in the process of natural gas migration along ancient reservoirs, with three sets of thick Mesozoic and Cenozoic mudstone or gypsum layers being effectively sealed and protected above.
Chaokun ZHANG , Mingyue GONG , Wei TIAN , Yanxin HE , Dongya ZHU , Lei WANG . Helium resource evaluation and enrichment model in Yakela area, Tarim Basin[J]. Natural Gas Geoscience, 2023 , 34(11) : 1993 -2008 . DOI: 10.11764/j.issn.1672-1926.2023.08.008
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