Chun Chang Huang

Biographic Data

ID	3646464
NAME	Chun Chang Huang
GIVEN NAMES	Chun Chang
FAMILY NAME	Huang
SIGNATURE	HUANG C C
AFFILIATIONS	Shaanxi Normal University
ORCID	0000-0001-8062-8217
VERIFIED	Yes
TOTAL WORKS	22
TOTAL CITATIONS	33
AUTHOR COUNT	22
EDITOR COUNT	0
FIRST PUBLICATION YEAR	2000
LATEST PUBLICATION YEAR	2026
H-INDEX	4

Human adaptation to the mid-Holocene hydroclimatic instability during the Miaodigou phase of the Yangshao culture within the Guanzhong Basin, middle Yellow River
Open AccessRunang Liu, Yuzhu Zhang et al.ARTICLEJournal of Archaeological Science…2026
Evolutionary history of a paleo-oxbow lake in the Yellow River within the Zoige Basin, NE Tibetan Plateau
Open AccessPengpeng Cao, Yuzhu Zhang et al.ARTICLEQuaternary International2025References: 1
Micromorphological evidence of pedogenesis and paleoclimatic change in the Holocene loess-paleosol in the south Qinling Mountains, China
Open AccessPeini Mao, Jiangli Pang et al.ARTICLEQuaternary International2021
Prehistoric and historic overbank floods in the Luoyang Basin along the Luohe River, middle Yellow River basin, China
Open AccessYuzhu Zhang, Chun Chang Huang et al.ARTICLEQuaternary International2019
Palaeoclimatic and palaeoenvironmental implications of late-Pleistocene aeolian sand in the Jin-Shaan Gorges of the Yellow River valley revealed by luminescence chronology
Open AccessYuzhu Zhang, Chun Chang Huang et al.ARTICLEThe Holocene2019References: 9
River valleys are critical water-gas-rock interactions zone, where close interaction between fluvial and aeolian deposition are a pronounced feature in arid, semi-arid, and semi-humid environments. Pedo-sedimentological investigations were carried out in the Jin-Shaan Gorges of the Yellow River valley. Two late-Pleistocene and Holocene aeolian sand-loess profiles were identified within the cliff riverbank. The aim of this study is to reveal the p…
Mid-late Holocene temperature and precipitation variations in the Guanting Basin, upper reaches of the Yellow River
Open AccessHui Zhao, Chun Chang Huang et al.ARTICLEQuaternary International2018
The linkages with fires, vegetation composition and human activity in response to climate changes in the Chinese Loess Plateau during the Holocene
Open AccessZhihai Tan, Yongming Han et al.ARTICLEQuaternary International2018
Identification of the prehistoric catastrophes at the Lajia Ruins using micromorphological analysis within the Guanting Basin, Minhe County, Qinghai Province
Open AccessYuzhu Zhang, Chun Chang Huang et al.ARTICLEArchaeological and Anthropological…2018Cited by: 4References: 26
Holocene palaeoflood events recorded by slackwater deposits along the Jin-shan Gorges of the middle Yellow River, China
Open AccessXiaogang Li, Chun Chang HuangARTICLEQuaternary International2017
Extreme paleoflood events 3200–3000 a BP in the Jingyuan–Jingtai reaches of the upper Yellow River, China
Open AccessGuiming Hu, Chun Chang Huang et al.ARTICLEThe Holocene2016Cited by: 1References: 10
A set of paleoflood slack water deposit (SWD) beds was identified within slope clasts at the Jinpingcun (JPC) site in the Jingyuan–Jingtai reaches of the upper Yellow River gorges based on sedimentary criteria and analytical results. Paleoflood hydrology methods were applied to reconstruct paleoflood events in the Jingyuan–Jingtai reaches. The paleoflood peak stages were calculated based on the highest end-point elevations of the SWDs. The HEC-RA…
Palaeo-earthquake and palaeo-mudflow events at the Machangyuan Ruins in the Huangshui River valley, northeastern margin of the Tibetan Plateau
Open AccessYongqiang Guo, Chun Chang Huang et al.ARTICLEThe Holocene2016References: 13
Palaeo-earthquake event recorded by loess rapture fissures (N30°–40°W and N40°–50°E trending) and palaeo-mudflow event recorded by red clay deposits were identified at the Machangyuan Ruins in the Huangshui River valley, at the foot of the northeastern Tibetan Plateau. Comparative analysis of grain-size distributions and geochemical elements of local outcrops indicates that the red mudflows were sourced from the gullies on the valley side where u…
Sedimentary records of palaeofloods in the Wubu Reach along the Jin-Shaan gorges of the middle Yellow River, China
Open AccessLongjiang Fan, Chun Chang Huang et al.ARTICLEQuaternary International2015
OSL dating of the massive landslide-damming event in the Jishixia Gorge, on the upper Yellow River, NE Tibetan Plateau
Open AccessYuzhu Zhang, Chun Chang Huang et al.ARTICLEThe Holocene2015Cited by: 2References: 9
Frequent natural hazards cause huge damage to human life and society in the mountainous regions along the eastern rim of the Tibetan Plateau. A massive landslide damming event has been reported in the Jishixia Gorge on the upper Yellow River as it emerges from the NE Tibetan Plateau. It was speculated that a breach of the dammed lake might have resulted in a super flood disaster that ruined the major Neolithic settlement at Lajia (4.20–3.95 ka BP…
Palaeoenvironmental implications of the prehistorical catastrophes in relation to the Lajia Ruins within the Guanting Basin along the Upper Yellow River, China
Open AccessChun Chang Huang, Jiangli Pang et al.ARTICLEThe Holocene2013Cited by: 1References: 4
Archaeological excavations have exposed a shocking picture of the prehistorical catastrophes in the Lajia Ruins in the upper Yellow River. The grouped skeletons resting on the dwelling floors show a vivid scene of the mortal struggle of human being during catastrophes. Geological records of the major disasters in relation to the devastation of this prehistorical settlement were investigated by detailed field observations, sedimentological analysi…
Wildfire history and climatic change in the semi-arid loess tableland in the middle reaches of the Yellow River of China during the Holocene
Open AccessZhihai Tan, Chun Chang Huang et al.ARTICLEThe Holocene2013Cited by: 1References: 8
High-resolution macroscopic charcoal and sediment analysis was used to reconstruct fire history and environmental changes from three loess-paleosol profiles on the semi-arid loess tableland landscape during the Lateglacial period and the Holocene. Analysis of charcoal concentrations, influx, and the ratios of particle-size classes (from which changes in charcoal taphonomy over time are inferred) in the profiles show spatially coherent patterns of…
Development of gully systems under the combined impact of monsoonal climatic shift and neo-tectonic uplift over the Chinese Loess Plateau
Open AccessChun Chang Huang, Jiangli Pang et al.ARTICLEQuaternary International2012
Comparative study of the modern flood slackwater deposits in the upper reaches of Hanjiang and Weihe River Valleys, China
Open AccessYuzhu Zhang, Chun Chang Huang et al.ARTICLEQuaternary International2012
Sedimentological study of the stratigraphy at the site of Homo erectus yunxianensis in the upper Hanjiang River valley, China
Open AccessYongqiang Guo, Chun Chang Huang et al.ARTICLEQuaternary International2012Cited by: 4References: 5
Holocene wildfires related to climate and land-use change over the Weihe River Basin, China
Open AccessZhihai Tan, Chun Chang Huang et al.ARTICLEQuaternary International2011
Sedimentary records of extraordinary floods at the ending of the mid-Holocene climatic optimum along the Upper Weihe River, China
Open AccessChun Chang Huang, Jiangli Pang et al.ARTICLEThe Holocene2011Cited by: 5References: 7
Sedimentary records of the Holocene extraordinary floods were investigated in the upper reaches of the Weihe River, a major tributary in the middle Yellow River basin. Palaeoflood slackwater deposits (SWD) were identified at several sites on the riverbanks. These clayey silt beds are inserted into the Holocene aeolian loess-soil profiles and slope clastic deposits. They have recorded the extraordinary palaeoflood events which occurred between 320…
Climate change and Zhou relocations in early Chinese history
Open AccessChun Chang Huang, Hongxia SuARTICLEJournal of Historical Geography2008Cited by: 8
A regional aridity phase and its possible cultural impact during the Holocene Megathermal in the Guanzhong Basin, China
Open AccessChun Chang Huang, Jie Zhou et al.ARTICLEThe Holocene2000Cited by: 7References: 1
Evidence of climatic variations and the impact of past farming was identified in a Holocene loess profile near Xi'an in the Guanzhong Basin, China. Detailed studies of the profile indicate that crop cultivation began at 7000 yr BP in the Neolithic and carried on to present in the area. Disturbance of the profile by cultivation has not masked evidence of changes in aeolian dust deposition and bio-pedogenic processes caused by climatic variations. …