We report a paleomagnetic investigation on Permian volcanic rocks in the middle-east Inner Mongolia, NE China, aiming to puzzle out the timing and position of the final closure of the eastern Paleo-Asian ocean (PAO) and further to better understand tectonic evolution of the Central Asian Orogenic Belt (CAOB). Two pre-folding characteristic components are isolated from the Sanmianjing and Elitu formations (~283–266 Ma) in the northern margin of the North China block (NMNCB) and the Dashizhai Formation (~280 Ma) in the Songliao-Xilinhot block (SXB), respectively
The formation of the Tibetan Plateau involved the opening and closing of multiple oceans (the ‘Tethy...
The Qinghai-Tibet Plateau comprises a mosaic of geologically distinct Paleozoic and Mesozoic terrane...
This paper presents new data from palaeomagnetic investigations on the Upper Palaeozoic and Mesozoic...
We report a paleomagnetic investigation on Permian volcanic rocks in the middle-east Inner Mongolia,...
The tectonic evolution of the Paleo-Asian Ocean between the North China Block (NCB) and the Mongolia...
International audienceThe tectonic evolution of the Paleo-Asian Ocean between the North China Block ...
A paleomagnetic study of late Paleozoic rocks in two areas of northwestern China helps to constrain ...
Different final closing ages have been proposed for the evolution of the Paleo-Asian Ocean (PAO), in...
International audienceThe Beishan Orogenic Belt plays an important role in understanding the Paleozo...
To provide further constraints on the tectonic transition and paleogeography of the southern Central...
The Paleo-Tethys Ocean was a major eastward-widening ocean that separated eastern Gondwana and easte...
The Solonker suture zone in the southeastern Central Asian Orogenic Belt is generally regarded as th...
International audienceWe conducted a paleomagnetic study on the Early Permian volcanic and sedimenta...
International audienceIn order to better understand the kinematics and geodynamics of the late Paleo...
International audienceWe present reconstructions of the Mongol-Okhotsk (MO) Ocean, based on a review...
The formation of the Tibetan Plateau involved the opening and closing of multiple oceans (the ‘Tethy...
The Qinghai-Tibet Plateau comprises a mosaic of geologically distinct Paleozoic and Mesozoic terrane...
This paper presents new data from palaeomagnetic investigations on the Upper Palaeozoic and Mesozoic...
We report a paleomagnetic investigation on Permian volcanic rocks in the middle-east Inner Mongolia,...
The tectonic evolution of the Paleo-Asian Ocean between the North China Block (NCB) and the Mongolia...
International audienceThe tectonic evolution of the Paleo-Asian Ocean between the North China Block ...
A paleomagnetic study of late Paleozoic rocks in two areas of northwestern China helps to constrain ...
Different final closing ages have been proposed for the evolution of the Paleo-Asian Ocean (PAO), in...
International audienceThe Beishan Orogenic Belt plays an important role in understanding the Paleozo...
To provide further constraints on the tectonic transition and paleogeography of the southern Central...
The Paleo-Tethys Ocean was a major eastward-widening ocean that separated eastern Gondwana and easte...
The Solonker suture zone in the southeastern Central Asian Orogenic Belt is generally regarded as th...
International audienceWe conducted a paleomagnetic study on the Early Permian volcanic and sedimenta...
International audienceIn order to better understand the kinematics and geodynamics of the late Paleo...
International audienceWe present reconstructions of the Mongol-Okhotsk (MO) Ocean, based on a review...
The formation of the Tibetan Plateau involved the opening and closing of multiple oceans (the ‘Tethy...
The Qinghai-Tibet Plateau comprises a mosaic of geologically distinct Paleozoic and Mesozoic terrane...
This paper presents new data from palaeomagnetic investigations on the Upper Palaeozoic and Mesozoic...