gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0265gtcrust-406Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSDISCUSSION ON THE RELATIONSHIP BETWEEN DEEP SEISMIC REFLECTION PATTERNS AND TECTONIC UNITS OF THE EASTERN PART OF THE CENTRAL ASIAN OROGENIC BELT IN NORTHEASTERN CHINADISCUSSION ON THE RELATIONSHIP BETWEEN DEEP SEISMIC REFLECTION PATTERNS AND TECTONIC UNITS OF THE EASTERN PART OF THE CENTRAL ASIAN OROGENIC BELT IN NORTHEASTERN CHINAHouH.HouH.

100037 Beijing

100037 Beijing

GaoR.GaoR.

100037 Beijing

100037 Beijing

KrönerA.KrönerR.

100037 Beijing;

55099 Mainz

100037 Beijing;

55099 Mainz

ZhangX.ZhangX.

College of Earth Science,

130061 Changchun

College of Earth Science,

130061 Changchun

ZhangS.ZhangS

State Key Laboratory of Biogeology and Environmental Geology, 

100083 Beijing

State Key Laboratory of Biogeology and Environmental Geology, 

100083 Beijing

Institute of Geology, Chinese Academy of Geological SciencesКитайInstitute of Geology, Chinese Academy of Geological SciencesChinaInstitute of Geology, Chinese Academy of Geological Sciences; Institute of Geosciences, University of MainzКитайInstitute of Geology, Chinese Academy of Geological Sciences; Institute of Geosciences, University of MainzChinaJilin UniversityКитайJilin UniversityChinaChina University of GeosciencesКитайChina University of GeosciencesChina20171110201783473474Copyright © Hou H., Gao R., Kröner A., Zhang X., Zhang S., 20172017Hou H., Gao R., Kröner A., Zhang X., Zhang S.Hou H., Gao R., Kröner R., Zhang X., Zhang S.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/406

Division of tectonic units in the eastern part of the Central Asian Orogenic Belt in northeast China has been a major concern and resulted in much fieldwork, but the division of these tectonic units in NE China is still controversial. Although detection of tectonic units in seismic sections is not straightforward, for this meeting, we shall try to relate tectonic units with the crustal and upper mantle structure and deformation derived from a ~2500 km long reflection seismic profile (Figure, red lines) in this area, recently acquired or reprocessed with support of China Geological Survey and the Chinese SinoProbe Project.

Division of tectonic units in the eastern part of the Central Asian Orogenic Belt in northeast China has been a major concern and resulted in much fieldwork, but the division of these tectonic units in NE China is still controversial. Although detection of tectonic units in seismic sections is not straightforward, for this meeting, we shall try to relate tectonic units with the crustal and upper mantle structure and deformation derived from a ~2500 km long reflection seismic profile (Figure, red lines) in this area, recently acquired or reprocessed with support of China Geological Survey and the Chinese SinoProbe Project.

ReferencesXu B., Zhao P., Wang Y., Liao W., Luo Z., Bao Q., Zhou Y., 2015. The pre-Devonian tectonic framework of Xing’an–Mongolia orogenic belt (XMOB) in north China. Journal of Asian Earth Sciences 97 (Part B), 183–196. https://doi.org/10.1016/j.jseaes.2014.07.020.Xu B., Zhao P., Wang Y., Liao W., Luo Z., Bao Q., Zhou Y., 2015. The pre-Devonian tectonic framework of Xing’an–Mongolia orogenic belt (XMOB) in north China. Journal of Asian Earth Sciences 97 (Part B), 183–196. https://doi.org/10.1016/j.jseaes.2014.07.020.

The authors declare that there are no conflicts of interest present.