乌拉特后旗测老庙坳陷下白垩统巴音戈壁组实测剖面简介——测老庙坳陷典型露头介绍之三
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本文为中陕核工业集团委托的研究项目“测老庙盆地区域地质研究与铀矿有利区带预测”的成果之一。


An Introduction to Stratigraphic Sections of the Lower Cretaceous Bayingebi Formation Surveyed in the Celaomiao Depression, Urad Rear Banner, Inner Mongolia——One of the Typical Outcrops in Celaomiao Depression for Earth Science Research and Field Training
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    摘要:

    本文描述了内蒙古自治区西部乌拉特后旗测老庙坳陷下白垩统巴音戈壁组的三条实测剖面,分别位于测老庙坳陷南缘西侧、南缘东侧和西北缘。其中,测老庙南缘西侧剖面出露了巴音戈壁组的主要部分,发育了一套完整的洪积扇相—河流相—湖泊相—河流相—洪积扇相的陆相沉积旋回。该剖面底部不整合覆盖在前寒武系变质基底之上,未见顶。南缘东侧发育了洪积扇相—辫状河相—洪积扇相沉积旋回,属于巴音戈壁组上段,其下部可能与南缘西侧剖面存在地层重复,而上部未见顶。测老庙坳陷西北缘剖面则出露了一套湖相页岩为主夹三角洲入湖砂体的地层,代表了巴音戈壁组的上段中部,其下部未见底,上部未见顶。由于该区植被稀少,剖面露头良好,这三条剖面可作为巴音戈壁盆地群陆相沉积体系研究的重要材料和区域地质野外测量实习的良好场所。

    Abstract:

    The Celaomiao Depression, the eastern part of Bayingebi Basins, is located in Chaogewendu’er Town, Wulatehouqi (Urad Rear Banner), Bayannur City, Inner Mongolia. The research is mainly focused on sedimentary environments of the Lower Cretaceous Bayingebi Formtaion. In this article three stratigraphical sections surveyed in the Celaomiao Depression have been demonstrated. The two outcrop cross sections are situated in the western side and eastern side of the depression along its southern margin respectively, and the other one is near the northwest margin of the depression. The scarcity of vegetation in the Celaomiao and wellexposed outcrops make the three sections be important places for geological research and field training.

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李莎,冯雪东,郑大燃,张琦,张海春,章雨旭,吕洪波.2017.乌拉特后旗测老庙坳陷下白垩统巴音戈壁组实测剖面简介——测老庙坳陷典型露头介绍之三[J].地质论评,63(6):1624-1638,[DOI].
LI Sha, FENG Xuedong, ZHENG Daran, ZHANG Qi, ZHANG Haichun, ZHANG Yuxu, LV Hongbo.2017. An Introduction to Stratigraphic Sections of the Lower Cretaceous Bayingebi Formation Surveyed in the Celaomiao Depression, Urad Rear Banner, Inner Mongolia——One of the Typical Outcrops in Celaomiao Depression for Earth Science Research and Field Training[J]. Geological Review,63(6):1624-1638.

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  • 收稿日期:2017-06-06
  • 最后修改日期:2017-07-22
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  • 在线发布日期: 2017-11-21
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