Results 91 to 100 of about 653,638 (207)

Orbital-scale precipitation variations in the western Qaidam Basin during the Late Pliocene: evidence from magnetic parameters and median grain-size [PDF]

open access: yesClimate of the Past
A recent study suggests that the precipitation records of the western Qaidam Basin during the middle Piacenzian warm period (mPWP, 3.264–3.025 Ma) are broadly consistent with those of the monsoon-influenced regions, and are highly sensitive to 20 kyr ...
Z. Luo   +10 more
doaj   +1 more source

Apatite fission track dataset of southwestern Qaidam Basin and western Altyn Tagh Range

open access: yes
This dataset include apatite fission track analyzed results of bedrock samples from the Altyn Tagh Range, and detrital apatite fission track analyzed results of Eocene to Miocene sedimentary samples from southwestern Qaidam Basin, northern Tibetan ...
Li, Bing
core   +1 more source

Cenozoic growth of the Eastern Kunlun Range (northern Tibetan Plateau): evidence from sedimentary records in the southwest Qaidam Basin

open access: yes, 2020
The Cenozoic sedimentary infill of the Qaidam Basin in the northern Tibetan Plateau provide significant insights into the uplift history and the tectonic evolution of the basin-bounding mountain ranges.
Guangwei Li (822910)   +5 more
core   +1 more source

Brain-terrain-like features in the Qaidam Basin: Implications for various morphological features on Mars

open access: yes, 2021
"Brain terrain" is a type of patterned ground composed of sinuous ridges and troughs. It is widespread in mid-high latitude regions on Mars and has been interpreted to be formed by sublimation of ground ice. In the Qaidam Basin, a geomorphological analog
He, H   +14 more
core   +1 more source

Basin-mountain tectonic pattern and hydrocarbon exploration domain in north margin of Qaidam Basin

open access: yes, 2008
Seismic profile crossing southern boundary of Saishiteng Mountain shows the shear tectonic characteristic of fault zone at southern boundary of Saishiteng Mountain.
Jun LI   +3 more
core   +1 more source

The relationship between groundwater and natural vegetation in Qaidam Basin

open access: yesJournal of Groundwater Science and Engineering, 2021
To accurately evaluate ecological risks trigged by groundwater exploitation, it must be clarified the relationship between vegetation and groundwater. Based on remote sensing data sets MOD13Q1, groundwater table depth (WTD) and total dissolved solids (TDS), the relationship between groundwater and natural vegetation was analyzed statistically in the ...
Xue-ya Dang   +3 more
openaire   +1 more source

Petrologic and geochemical characteristics of high-quality saline lacustrine source rocks in western Qaidam Basin

open access: yesPetroleum Research, 2018
The main oil source in western Qaidam Basin is the Paleogene saline lacustrine source rocks. Traditionally, it was considered that these source rocks were characterized by low abundance and poor type of organic matter as well as limited oil generation ...
Bin Zhang   +5 more
doaj   +1 more source

Pollen assemblages and their environmental implications in the Qaidam Basin, NW China

open access: yes, 2012
The Qaidam Basin is one of the most sensitive areas to climate change in China, owing to its unique geographical position and ecological condition. In this study, 32 surface-soil pollen samples were collected to reveal the relationship between modern ...
Manyue Li   +16 more
core   +1 more source

Lacustrine algal limestone reservoir in western Qaidam Basin, China [PDF]

open access: yes, 2015
Compared to marine carbonate around the world, lacustrine carbonate is relatively scarce. Much less attention has been paid to it. Lacustrine carbonate, a product of mixed deposition of continental clastics and carbonate under special conditions, can be ...
Zhao, Fan
core  

Environmental Evolution Recorded by Tamarix Nebkhas in the Qaidam Basin

open access: yesWater
A typical Tamarix nebkha was studied in the southern Qaidam Basin, China. K-feldspar pIRIR dating was applied to establish a reliable chronological framework, and an Undatable age–depth model was constructed. Accumulation rates (AR) declined in stages: rapid (~1.33 cm/a; ~370–260 yr BP), slower (~0.75 cm/a; ~260–130 yr BP), and slowest (~0.31 cm/a ...
Yongxin Zeng   +5 more
openaire   +1 more source

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