QUATERNARY CLIMATE-CHANGE AND THE FORMATION OF RIVER TERRACES ACROSS GROWING ANTICLINES ON THE NORTH FLANK OF THE TIEN-SHAN, CHINA

Nested stream terraces, warped upward over actively growing anticlines along the north flank of the Tien Shan in western China, appear to re cord alternating phases of valley widening and incision. Differences o f relative heights between remnants of four separate strath terraces a long one river and between two such terraces along another reach 100 t o 120 m over the crests of the anticlines. We infer that this spacing is due to alternating stages of valley widening and rapid incision ass ociated with climate changes with a periodicity of 100 kyr. The crests of the anticlines appear to emerge from the aggrading flanks of the a nticlines at an average rate of about 1 mm/a. The maximum heights of 2 5 and 35 (+/-10) m for the lowest terraces above their projected initi al profiles imply ages of roughly 25 kyr and 35 kyr (+/-10 kyr). Hence , they suggest that flood plains, which were abandoned to form the ter races, developed adjacent to active stream beds during the last glacia l period, when climates were relatively cold and dry. We presume that they were incised during deglacial periods when discharges and stream power increased. Apparent durations of exposure, obtained from Be-10 i n quartz cobbles lying on the surface of the lower terrace from one an ticline, concur with abandonment and deep (similar to 150 m) incision of the flood plain during the last global deglaciation (ca. 20 to 13 k yr B.P.). A minimum carbon-14 date of 33.9 kyr B.P. from deposits on t he lowest terrace sequence from the other anticline, however, implies that such abandonment and incision of this flood plain occurred before the most recent global glacial maximum, about 20 kyr B.P. We infer th at incision of this second anticline's floodplain began during an earl ier deglacial epoch within the last glacial period (between about 70 a nd 20 kyr, and perhaps near 35 kyr B.P.).