Study of the Late Quaternary Slip Rate along the Northern Segment on the South Branch of Longling-Ruili Fault
///Based on interpretation of remote sensing images, quantitative geomorphologic deformation measurement and dating of young terrace deposits and alluvial fans, the paper obtains some new results as follows: the northern segment of Longling-Ruili Fault is a Holocene dextral strike-slip fault with a normal slip component. The terrace T1 composed mainly of alluvial deposits formed during 4 ka B.P. was offset by the northern segment of the Longling-Ruili Fault, with left-lateral and vertical displacements of 8~