宋立军, 牟秋环, 李爱荣, 李莉. 宁夏固原炭山窑山组形成时代的裂变径迹热史约束[J]. 煤田地质与勘探, 2013, 41(4): 1-4. DOI: 10.3969/j.issn.1001-1986.2013.04.001
引用本文: 宋立军, 牟秋环, 李爱荣, 李莉. 宁夏固原炭山窑山组形成时代的裂变径迹热史约束[J]. 煤田地质与勘探, 2013, 41(4): 1-4. DOI: 10.3969/j.issn.1001-1986.2013.04.001
SONG Lijun, MU Qiuhuan, LI Airong, LI Li. Fission-track thermal evolution history in the formation age of Yaoshan Formation[J]. COAL GEOLOGY & EXPLORATION, 2013, 41(4): 1-4. DOI: 10.3969/j.issn.1001-1986.2013.04.001
Citation: SONG Lijun, MU Qiuhuan, LI Airong, LI Li. Fission-track thermal evolution history in the formation age of Yaoshan Formation[J]. COAL GEOLOGY & EXPLORATION, 2013, 41(4): 1-4. DOI: 10.3969/j.issn.1001-1986.2013.04.001

宁夏固原炭山窑山组形成时代的裂变径迹热史约束

Fission-track thermal evolution history in the formation age of Yaoshan Formation

  • 摘要: 查明鄂尔多斯盆地西缘窑山组的形成时代,是正确进行地层对比、恢复盆地原貌及其演化的关键。根据"随着沉积作用的进行,窑山组埋藏深度增加,其经历的温度相应增加"的原理,运用磷灰石裂变径迹热史模拟方法,重建了宁夏固原炭山窑山组样品经历的温度史。热史模拟结果表明,样品初始埋藏增温的时间是距今196 Ma,样品埋藏增温的时间区间距今196~168 Ma。从而可知,炭山窑山组样品形成于距今196 Ma,窑山组形成于早-中侏罗世延安期(距今196~168 Ma)。

     

    Abstract: To identify the formation age of Yaoshan Formation is the key to carry out stratigraphic division and correlation, to reconstruct prototype basin and to evaluate regional resources in west margin of Ordos basin. With the development of sedimentation, the temperature of Yaoshan Formation increased gradually with the increase of the buried depth. The fission track thermal history simulation result of sandstone samples from Yaoshanzu Formation in Tanshan demonstrates that the initial burial warming time was 196 Ma and the burial warming time was between 196 Ma and 168 Ma. It shows Yaoshan Formation was deposited between 196 and 168 Ma in early-middle Jurassic.

     

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