摘要：Zircon (U-Th)/He thermochronometry was used as an effective indicator to study the thermal history of deep sedimentary basins with high temperatures. Zircon He ages and closure temperatures are very important parameters. In this paper, detrital zircon He closure temperature was studied by establishing the evolutionary pattern between zircon He ages and burial depth of borehole samples obtained from the Cenozoic strata in the Bohai Bay and Tarim basins, which have different thermal settings. The results show that the zircon He closure temperature of natural evolution samples is 200°C, which is higher than the temperature obtained from thermal simulation experiments (183°C). The temperature range of 140–200°C corresponds to the zircon helium partial retention zone. By properly understanding zircon He closure temperatures, zircon (U-Th)/He thermochronometry can provide a correct explanation of the He ages, and significant guidance in the study of the evolution of source rocks and the process of hydrocarbon accumulation in deep sedimentary basins.
© 2019, Science China Press and Springer-Verlag GmbH Germany, part of Springer Nature.

ISSN号：1674-7313

卷、期、页：v 63,n 3,p412-424

发表日期：2020-03-01

影响因子：3.241900

期刊分区（SCI为中科院分区）：二区

收录情况：SCIE（科学引文索引网络版）,EI（工程索引）

发表期刊名称：Science China Earth Sciences

参与作者：李慧莉,Stockli, Daniel F.

通讯作者：蔡长娥,蔡长娥,刘念

第一作者：邱楠生,常健

论文类型：期刊论文

论文概要：蔡长娥,蔡长娥,邱楠生,李慧莉,Stockli, Daniel F.,常健,刘念，Study of the closure temperature of (U-Th)/He in detrital zircon obtained from natural evolution samples，Science China Earth Sciences，2020，v 63,n 3,p412-424

论文题目：Study of the closure temperature of (U-Th)/He in detrital zircon obtained from natural evolution samples