Results 11 to 20 of about 206 (165)
The Yangtze Craton in South China is generally regarded as an Archean‐Paleoproterozoic continental nucleus with a coherent basement that collided with the Cathaysia Block in the Early Neoproterozoic.
Xiaofan Deng +7 more
doaj +2 more sources
The deep boundary and contact relationship between the Yangtze and Cathaysia Blocks (the major tectonic units of the Southern China Block), as well as the tectonic attributes of the Jiangnan Orogenic Belt, have remained unknown or controversial.
Rubing Han +7 more
doaj +1 more source
The southeastern Tibetan Plateau, which includes the Tibetan Plateau, Yangtze Block, and Cathaysia Block, is geotectonically situated in the compound part of the Tethys-Himalayan tectonic domain and the Peninsular Pacific tectonic domain.
Jing Liu +8 more
doaj +1 more source
Recent seismic studies presented evidence for mantle upwelling and magmatic intrusions in the Cathaysia Block in South China. However, the key evidence or crustal velocity structure to understand crustal magma chambers that contributed to ore ...
Jiawei Li, Chuansong He, M. Santosh
doaj +1 more source
The outline of the Proterozoic South China Ocean
The geological circle has been studying the South China Ocean for 40 years. Based on the existing studies, the geological features of the middle Neogene South China Ocean and related geological structures and mineralization issues have been further ...
YANG Minggui +5 more
doaj +1 more source
Amalgamation of the Yangtze and Cathaysia blocks in the context of Gondwana assembly in the early Paleozoic has been addressed for decades, but the far-field effects on the Yangtze Block during the amalgamation remain unclear.
Hao Tang +8 more
doaj +1 more source
By harmonically fitting the arrival times of the P‐to‐S converted phases from the Moho, we systematically investigate the crustal anisotropy beneath the Cathaysia Block (CaB) and the surrounding areas in South China for the first time.
Mengkui Li +3 more
doaj +1 more source
Upwelling mantle beneath the Cathaysia Block, South China
The raw data is used to image upper mantle discontinuities beneath the South China Block.
Chuansong, He, Santosh, M.
openaire +3 more sources
The thermal-rheological structure of the continental lithosphere is an important indicator of geodynamic processes. Tectonic compression and extension may change thermal-rheological structure of lithosphere. However, the thermal-rheological evolution over geological time may be difficult to determine because of overprints of subsequent geological ...
Gan, Haonan +3 more
openaire +1 more source
Late Oligocene Formation of the Pearl River Triggered by the Opening of the South China Sea
The Pearl River is one of the largest rivers entering the South China Sea, yet its initiation time remains debated, a topic we address using Pb isotopes in detrital K‐feldspar.
Zengjie Zhang +7 more
doaj +1 more source

