18 results on '"Cao, Liwan"'
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2. Paleomagnetic and geochronological results of the Risong Formation in the western Lhasa Terrane: Insights into the Lhasa-Qiangtang collision and stratal age
3. Orbital forcing of Triassic megamonsoon activity documented in lacustrine sediments from Ordos Basin, China
4. Late Ordovician obliquity-forced glacio-eustasy recorded in the Yangtze Block, South China
5. Cyclostratigraphy of the global stratotype section and point (GSSP) of the basal Guzhangian Stage of the Cambrian Period
6. Astronomical calibration of the Middle Ordovician of the Yangtze Block, South China
7. Magnetic response to air pollution recorded by soil and dust-loaded leaves in a changing industrial environment
8. Magnetic properties of tree leaves and their significance in atmospheric particle pollution in Linfen City, China
9. Paleomagnetic Constraints on the India–Asia Collision and the Size of Greater India
10. Paleomagnetism of the Late Cretaceous Red Beds From the Far Western Lhasa Terrane: Inclination Discrepancy and Tectonic Implications
11. Paleomagnetic Constraints on the Origin and Drift History of the North Qiangtang Terrane in the Late Paleozoic
12. Paleomagnetic and Geochronological Results From the Zhela and Weimei Formations Lava Flows of the Eastern Tethyan Himalaya: New Insights Into the Breakup of Eastern Gondwana
13. A Stable Southern Margin of Asia During the Cretaceous: Paleomagnetic Constraints on the Lhasa-Qiangtang Collision and the Maximum Width of the Neo-Tethys
14. Paleomagnetic and Geochronologic Results of Latest Cretaceous Lava Flows From the Lhasa Terrane and Their Tectonic Implications
15. An economic passive sampling method to detect particulate pollutants using magnetic measurements
16. Efficiency of stepwise magnetic-chemical site assessment for fly ash derived heavy metal pollution
17. Atmospheric pollution history at Linfen (China) uncovered by magnetic and chemical parameters of sediments from a water reservoir
18. Paleoclimatic implications of magnetic susceptibility in Late Pliocene–Quaternary sediments from deep drilling core SG‐1 in the western Qaidam Basin (NE Tibetan Plateau)
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