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    1∶500 000二连–东乌旗成矿带西乌旗和白乃庙地区地质图空间数据库

    1∶500 000 Geological Map Spatial Database of the Xiwuqi and Bainaimiao Areas in the Erlian– Dongwuqi Metallogenic Belt

    • 摘要: 1∶500 000二连–东乌旗成矿带西乌旗和白乃庙地区地质图空间数据库的建设依托2016–2018年实施的中国地质调查局地质调查项目“二连–东乌旗成矿带西乌旗和白乃庙地区地质矿产调查”开展。古生代、中生代、古近纪及新近纪地层以组为单位,侵入岩时代以最新获取的777个LA-ICPMS和SHRIMP 锆石U-Pb年龄为依据,按照“岩性+时代”方法表达。地质图空间数据库的数据量为210 MB,包括地层面图元4682个,侵入岩面图元1938个。所有地质图面图元和同位素年龄点均建立了相应的属性。在编图过程中主要取得了如下成果: 结合生物区系和重要构造边界重新划分了古生代地层分区,新建、重新厘定了关键地层单位,完善了古生代地层格架; 重新厘定了区内古生代侵入岩时空分布及性质,早、晚古生代2阶段岩浆作用是对早、晚古生代2期俯冲增生造山作用的响应; 新识别并在图上表达出早古生代萨音敖包、昌图及晚古生代二道井–迪彦庙、乌兰沟等蛇绿混杂岩,较为细致地刻画了早古生代大洋南北双向俯冲形成的增生造山带结构,对晚古生代洋盆的俯冲与封闭进行了限定,重新划分了构造单元。这些成果和资料对兴蒙造山带研究过程中的古生代构造单元划分、晚古生代构造背景等具有较大分歧的科学问题具有限定作用。该空间数据库是目前兴蒙造山带中段资料最齐全、最新的1∶500 000地质图数据库,反映了本区地质调查和科学研究的最新成果。

       

      Abstract: The 1∶500 000 Geological Map Spatial Database of the Xiwuqi and Bainaimiao Areas in the Erlian-Dongwuqi Metallogenic Belt is developed as part of China Geological Survey’s project ‘Geological and Mineral Survey of the Xiwuqi and Bainaimiao Areas in the Erlian-Dongwuqi Metallogenic Belt’ during 2016 to 2018. The stratum of the Paleozoic, Mesozoic, Paleogene and Neogene are divided into different formations, while the intrusive rocks are expressed in the form of ‘lithology + era’ based on 777 LA-ICPMS and SHRIMP zircon U–Pb ages. The geological map spatial database is rich in geological information with a data size of 210 MB, including 4682 stratigraphic and 1938 intrusive rock surface entities, all of which are associated with their corresponding attributes. The following achievements have been made during the mapping process: the Paleozoic stratigraphic division has been revised considering biota and key tectonic boundaries, with newly established and re-defined important stratigraphic units and an improved Paleozoic stratigraphic framework; the temporal-spatial distribution and properties of Paleozoic intrusive rocks have been clarified, with the Early and Late Paleozoic two-stage magmatism being responses to corresponding subduction-accretion orogeny; newly identified ophiolitic mélanges, such as Early Paleozoic Sayin Aobao, Changtu and Late Paleozoic Erdaojing-Diyanmiao and Wulangou, have been expressed on the map, which shows the structure of the accretionary orogeny formed by the Early Paleozoic North and South bi-direction subduction. The final closure of the Paleo Asian ocean at the end of the Late Paleozoic was constrained and the tectonic units were re-divided. These achievements and data may shed light on scientific issues with diverging views regarding the Xing’an–Mongolian orogeny, such as the division of the Paleozoic tectonic units and late Paleozoic tectonic setting. As the latest and most complete 1∶500 000 geological map database in the middle part of the Xing’an–Mongolian orogeny so far, this spatial database reflects the latest achievements of geological surveys and research in this area.

       

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