Official Journal of the Asia Oceania Geosciences Society (AOGS)
Trenches | Sample number | Measured radiocarbon age | Calibrated ages cal AD | Mean (µ) | References |
---|---|---|---|---|---|
Hajipur | Â | Â | Â | Â | Malik et al. (2010a) |
 Undeformed unit | JMT6 | 300 ± 40 | 1426–1700 | 1707 |  |
Kangra | Â | Â | Â | Â | Â |
 Undeformed unit | JNMPC10 | 110 ± 30 | 1681–1938 | 1817 | Malik et al. (2015) |
Bhatpur | Â | Â | Â | Â | Kumahara and Jayangondaperumal (2013) |
 Undeformed unit | BHA-117 | 480 ± 40 | 1327–1476 | 1429 |  |
Chandigarh | Â | Â | Â | Â | Kumar et al. (2006) |
 Undeformed unit | PAN-03 | 665 ± 40 | 1270–1397 | 1333 |  |
Kala Amb | Â | Â | Â | Â | Kumar et al. (2001) |
 | C18 | 620 ± 30 | 1292–1401 | 1346 |  |
 | C15 | 420 ± 40 | 1420–1630 | 1492 |  |
Rampur Ganda | Â | Â | Â | Â | Kumar et al. (2006) |
 Undeformed unit | AB08 | 530 ± 35 | 1316–1443 | 1393 |  |
Lal Dang | Â | Â | Â | Â | Kumar et al. (2006) |
 Undeformed unit | LDT-31 | 375 ± 25 | 1447–1631 | 1526 |  |
Ramnagar | Â | Â | Â | Â | Kumar et al. (2006) |
 Undeformed unit | BR-06 | 695 ± 35 | 1444–1634 | 1526 |  |
Ramnagar | Â | Â | Â | Â | Rajendran et al. (2015) |
 Undeformed unit | P-1 | 727 ± 16 | 1264–1287 | 1276 |  |
Kaladungi | Â | Â | Â | Â | Malik et al. (2016) |
 Deformed unit | GDC06 | 80 ± 30 | 1690–1926 | 1826 |  |
 Undeformed unit | GDC010 | 250 ± 30 | 1521–1939 | 1676 |  |
Koliabas | Â | Â | Â | Â | Mugnier et al. (2005) |
 Deformed River Terrace | AA50068 | 775 ± 35 | 1190–1285 | 1246 |  |
Mahara |  |  |  |  | Lavé et al. (2005) |
 Undeformed unit | M2-12 | 880 ± 40 | 1036–1245 | 1143 |  |
Sir Khola | Â | Â | Â | Â | |
 | SIR08-05 | 645 ± 35 | 1280–1398 | 1340 |  |
Panijhora | Â | Â | Â | Â | Mishra et al. (2016) |
 Deformed | P10 | 990 ± 30 | 989–1153 | 1060 |  |
Chalsa | Â | Â | Â | Â | Kumar et al. (2010) |
 Deformed | C-7 | 840 ± 30 | 1059–1264 | 1201 |  |
Nameri | Â | Â | Â | Â | Kumar et al. (2010) |
 Deformed | N-22 | 895 ± 35 | 1039–1215 | 1126 |  |
Harmutty | Â | Â | Â | Â | Kumar et al. (2010) |
 | H13S | 670 ± 35 | 1270–1394 | 1330 |  |