SEDIMENTARY LANDSCAPE AND PALEO-LANDSCAPES OF AN ACTIVE ENDORHEIC FORELAND BASIN: THE JUNGGAR BASIN (XINJIANG, CHINA)
Résumé
The sedimentary landscape and dynamics of foreland basins, which are shaped by the interplays
between tectonics, climate, sedimentation and erosion processes, are key elements to
reconstruct the evolution of orogenic systems. Therefore, a detailed understanding of the relationships
between the foreland landscapes and these processes is necessary to improve our
knowledge on the sedimentary record in compressive regions. In this study, we focus on the
characterization of the present-day and palaeo-landscapes of an endorheic foreland basin where
deformation, sedimentation and erosion are still active and easily observable: the Junggar Basin
located in Central Asia. The interest of this basin resides in outstanding outcrops of its sedimentary
series and structures, numerous surface and subsurface data (satellite images, digital
topography, seismic profiles and drilling well data), and marked continental paleo-geographic
changes through the Cenozoic. The methodology consists in coupling different approaches (geomorphology,
sedimentology, sequential stratigraphy and structural geology) to characterize these
paleo-geographic changes across space and through time. As a starting point, we drew a morphosedimentological
map of the present-day landscape from the surface data to describe the current
drainage organization and associated sedimentary environments in the basin. Then, we estab- lished
several paleo-geographic maps from the surface and subsurface data to reconstruct the spatiotemporal
landscape evolution since 65 Ma. In the light of previous quantifications of its control
parameters (substratum deformation and sediment supplies), this evolution provides new qualitative
and quantitative constraints on landscape architecture and dynamics in continental foreland
contexts.