关键词: 中国东北早古生代造山带；索伦－西拉沐伦－长春缝合带；吉黑高压变质带；东北复合地块；大地构造学

Abstract:

The basement rocks in parts of NE China constitute a khondalitic sequence of sillimanite-and garnet-bearing gneisses, hornblende-plagioclase gneiss and various felsic paragneisses. Zircon U-Pb dating of garnet-sillimanite gneiss samples from the Erguna, Xing’an, Jiamusi and Khanka blocks all indicate that high-grade metamorphism occurred at ~500 Ma. Evidence from detrital zircons in Paleozoic sediments from the Songliao block also indicates the former presence of a ~500 Ma component. This uniformity of U-Pb ages across all crustal blocks in NE China establishes a>1 300 km long Late Pan-African khondalite belt with Pan-African syn-collisional granite, which we named here the ‘NE China Pan-African Orogen’.This indicates the blocks of NE China were amalgamated prior to ~500 Ma, contrary to current belief. One scenario is that this amalgamated terrane had a tectonic affinity to the Siberia craton, once forming part of the Late Pan-African (~500 Ma) Sayang-Baikal orogenic belt extensively developed around the southern margin of the Siberia craton. This belt was the result of collision between currently unidentified terranes with the Southeastern Angara-Anabar Province at about 500 Ma, where the rocks were deformed and metamorphosed to granulite facies. It appears likely that at sometime after ~450 Ma, the combined NE China blocks rifted away from Siberia and moved southward to form what is now NE China. The combined block collided with the North China craton along the Solonker-XarMoron-Changchun suture zone at ~230 Ma rather than in the end-Permian as previously thought. Local rifting at the eastern extremity of the developing Central Asian orogenic belt (CAOB) resulted in the splitting away of the Jiamusi/Khanka(/Bureya) blocks. However, this was only transient and sometime between 210 and 180 Ma, and these were re-united with the CAOB by the onset of Pacific plate subduction, which we named here the “Jilin-Heilongjiang high pressure belt” and forming which has dominated the tectonic evolution of the region since that time.

Key words: NE China Ealy-Paleozoic orogen, Solonker-XarMoron-Changchun suture zone, Ji-Hei HP belt, combined NE China plates；tectonics