supported by a grant from the Natural Science Foundation of China (No.41972051);the Fundamental Research Funds for the Central Universities,China University of Geosciences (Wuhan)(No.CUG190627)
In this study,a tremolite marble from the Dabie ultrahigh-pressure(UHP)terrane,eastcentral China was investigated for its metamorphic evolution by focusing on zircon.The marble contains an amphibolite-facies assemblag...
supported by the National Natural Science Foundation of China (Nos. 41572039, 41772054, and 41372076);the Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) (No. CUGQYZX1704)
Syn-collapse magmatism is a critical issue for evolution of the continental orogen.The Dabie Orogen is a typical orogen which was suffered from a complete collapse.Two kinds of granitoids,namely,the coarse-grained dio...
supported by the National Basic Research Program of China (No. 2015CB856101);the National Natural Science Foundation of China (Nos. 41372076 and 41572039);the Natural Science Foundation of Hubei Province (No. 2015CFB190)
The plate affiliation of the North Dabie terrane (NDT) has been controversial. To address this fundamental question, an integrated study of internal structure, in-situ U-Pb dating and trace element analysis in zirco...
supported by the National Natural Science Foundation of China(Nos.40372094 and 49972067)
Two fresh types of eclogites, namely the massive eclogite and foliated eclogite, are dis- cernible in large eclogite bodies surrounded by country rock gneisses from the Dabie Sulu UHP metamorphic zone. They are diffe...
The Dabie complex (DC) and the Tongbai complex (TBC) are separately distributed in the middle and eastern parts of the Qinling-Tongbai-Dabie orogenic belt. In this study, the Dabie complex can be divided into two unit...
This paper is supported by the NNSF of China( Nos.497940 41; 49772 14 6and49972 0 67) and Major State Basic Research Developme
The present day observed tectonic framework of ultrahigh pressure (UHP) metamorphic belt in the Dabie Sulu region was dominantly formed by an extensional process at 200-170 Ma, under amphibolite facies conditions, f...
The regional extent and spatial distribution of ultrahigh pressure metamorphic(UHPM) and high pressure metamorphic (HPM) rocks, and the geometrical relationships of various petrotectonic units in the Dabie-Sulu region...
The present-day observed crustal-scale tectonic style of ultrahigh-pressure metamorphic (UH-PM) and high-pressure metamorphic (HPM ) belts in the Dabie-Sulu region was dominantly formedby extensional processes, postda...
Structural studies in the Dabie massif show that distribution of strain is extremely heterogeneous and illustrates the pattern of deformation partitioning in the ultra high pressure (UHP) metamorphic province on all ...