Use of ground‐penetrating radar to investigate feathery complex linear dunes in the Kumtagh Desert, North‐west China

Abstract

The Kumtagh Desert, the last desert in China to be explored, contains a distribution of feathery dunes, a type of complex linear dune composited by linear dunes and lingoid zibars. A debate about the existence, underlying relief and formation process of these dunes has been ongoing since 1974. The authors use ground‐penetrating radar (GPR) images across dunes and interdune areas to better understand the shallow underlying relief and sedimentary structure of the dunes in the Kumtagh Desert. The results are compared with adjacent outcrops and exposures in an excavated trench. No evidence was found for underlying relief, such as yardangs, consistent with the trend and distribution of linear dune ridges that might have controlled the orientation of the dune. However, outcrop observation and remote sensing investigation indicate little gravel bar topography across or along the dunes. Lingoid zibars are common in interdune corridors. Sedimentary structures imaged by GPR in the zibar dunes indicate low‐angle strata dipping towards the SW, indicative of sand accumulation on the leeside of the lingoid zibar with dune migration towards the SW. Strata within the linear dunes are less well‐resolved but are interpreted to indicate a bimodal dip that has been recognized in previous studies of linear dunes.

Unravelling raked linear dunes to explain the coexistence of bedforms in complex dunefields

“…Raked linear dunes have been recognized for the first time in the Kumtagh desert 17 (Xinjiang province, China), where they cover an area of more than 2.4 × 10 4 km 2 . This remote and arid region of China has been the subject of intensive investigation in recent years 18 19 20 21 22 . These studies provide unique sets of data, but none of them have identified the mechanism for dune formation and the subsequent dune morphodynamics.…”