financially supported by Mobility project of Czech Ministry of Education,Youth and Sports and Ministry of Science and Technology of the People’s Republic of China(8H17050);institutional support of Inst.Geol.Czech Acad.Sci.(RVO67985831);the Strategic Priority Research Program of Chinese Academy of Sciences(XDB26000000);China-Czech 42th Inter-Governmental S&T Cooperation Project(42-3);the National Natural Science Foundation of China(41572006,41688103,41972007);UNESCO/IUGS/IGCP 679 project.
The Purbeck beds in Dorset, the Tuchengzi Formation in western Liaoning Liaoning Province or the Houcheng Formation in northern Hebei Province are non-marine Jurassic/Cretaceous (J/K) boundary sequences. A Czech-China...
Although Plate Tectonics cannot be effectively tested by palaeomagnetism in the Precambrian aeon due to the paucity of high precision poles spanning such a long time period,the possibility of Lid Tectonics is eminentl...
supported under a DST (ESS/16/290/2006) grant sanctioned to Santosh Kumar
Occurrence of mafic dykes in Himalaya has been intriguing and debated since long because of its difficulty to ascent and emplacement through a thickened crust.Mafic dykes in Kumaun Lesser Himalaya(KLH)of central Indian
Quasi-integrity of continental crust between Mid-Archaean and Ediacaran times is demonstrated by conformity of palaeomagnetic poles to near-static positions between -2.7-2.2 Ga, -1.5-1.2 Ga and -0.75-0.6 Ga. Interveni...
In carboniferous and triassic metacarbonates (anchizone to lower greenschist facies) of the Tethyan Himalayas the characteristic remanent magnetisations are carried by magnetite (ChRM\-1) and pyrrhotite (ChRM\-2;Kloot...
In Mesozoic carbonates of the Tethyan Himalayas two characteristic remanent magnetisations(ChRM\-1 and ChRM\-2)were identified by their unblocking spectra.The ChRM\-1 is carried by pyrrhotite(unblocking spectra:270~...
The research was supported by the National Natural Science Fundation of China (Grant No:48970070)
In western Henan, Late Palaeozoic coal measures are completely developed and well exposed. A great deal of research work on biostratigraphy was done by predecessors. After systematic palaeomagnetic studies, we have co...