Zhongshan Shen

ORCID: 0000-0002-0804-0950
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About
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Research Areas
  • Geology and Paleoclimatology Research
  • Geological and Geochemical Analysis
  • Geomagnetism and Paleomagnetism Studies
  • Silicon Carbide Semiconductor Technologies
  • Planetary Science and Exploration
  • Copper Interconnects and Reliability
  • Geological and Geophysical Studies
  • Semiconductor materials and devices
  • earthquake and tectonic studies
  • Paleontology and Stratigraphy of Fossils
  • Ferroelectric and Piezoelectric Materials
  • Geological formations and processes
  • Thin-Film Transistor Technologies
  • Electronic and Structural Properties of Oxides
  • Acoustic Wave Resonator Technologies
  • Astro and Planetary Science
  • Geochemistry and Elemental Analysis
  • Methane Hydrates and Related Phenomena
  • Zeolite Catalysis and Synthesis
  • Polar Research and Ecology
  • Isotope Analysis in Ecology
  • Supercapacitor Materials and Fabrication
  • ZnO doping and properties
  • Spaceflight effects on biology
  • Semiconductor materials and interfaces

Chinese Academy of Sciences
2016-2025

Institute of Geology and Geophysics
2020-2025

University of Chinese Academy of Sciences
2020-2025

Institute of Semiconductors
2016-2018

Dalian Institute of Chemical Physics
2002

Argonne National Laboratory
1993-1994

The evolution of the lunar magnetic field can reveal Moon’s interior structure, thermal history, and surface environment. mid-to-late-stage is poorly constrained, thus, existence a long-lived dynamo remains controversial. Chang’e-5 mission returned heretofore youngest mare basalts from Oceanus Procellarum uniquely positioned at midlatitude. We recovered weak paleointensities ~2 to 4 microtesla basalt clasts 2 billion years ago, attesting longevity until least midstage. This paleomagnetic...

10.1126/sciadv.adp3333 article EN cc-by-nc Science Advances 2025-01-01

The India-Asia collision is an outstanding smoking gun in the study of continental dynamics. How and when occurred remains a long-standing controversy. Here we present two new paleomagnetic data sets from rocks deposited on distal part Indian passive margin, which indicate that Tethyan Himalaya terrane was situated at paleolatitude ∼19.4°S ∼75 Ma moved rapidly northward to reach ∼13.7°N ∼61 Ma. This implies rifted India after Ma, generating North Sea. We document two-stage collision, first...

10.1093/nsr/nwaa173 article EN cc-by National Science Review 2020-07-24

The enigmatic geodynamic processes involved in the India-Asia collision shape our understanding of uplift and deformation Tibetan Plateau subsequent changes land-sea distribution pattern, monsoon-arid environments biotic evolution Central-Eastern Asia. However, current models dealing with history exhibit significant discrepancies how, when where exactly India Asia occurred. Recently, we proposed a new hypothesis that favored opening closure North Sea during late Cretaceous to Paleogene. Here...

10.1016/j.gloplacha.2022.103821 article EN cc-by Global and Planetary Change 2022-04-21

Ordered mesoporous carbons composed of arrays nanotubes have been synthesized using ordered silica templates via catalytic chemical vapor deposition. The possess bimodal pores, namely, the pores arise from "replica" frameworks template and correspond to carbon formed in channels (see Figure).

10.1002/1521-4095(20021203)14:23<1776::aid-adma1776>3.0.co;2-a article EN Advanced Materials 2002-12-03

Abstract The Tibetan Plateau accommodated major upper crustal shortening during Indian Plate oceanic and continental lithosphere subduction. Deciphering whether was continuous or episodic, how it correlates to geodynamic changes is challenging. Here we apply anisotropy of magnetic susceptibility (AMS), a sensitive synsedimentary strain indicator, ~3 km thick magnetostratigraphically dated sedimentary section (69–41.5 Ma) in eastern Tibet. AMS shows “earliest deformation” fabrics from 69–52...

10.1029/2020gl087531 article EN Geophysical Research Letters 2020-04-10

Abstract Oceanic red beds, preserving primary depositional remanent magnetization, play a key role in reconstructing the Tethyan paleogeography. However, partial remagnetization caused by chemical processes could be pervasive these rocks, leading to flawed reconstructions, and thus, differentiating secondary remanences is important. In this paper, we conduct multiple X‐ray diffraction, petrographic, diffuse reflectance spectroscopy, rock magnetic analyses on Upper Cretaceous oceanic beds...

10.1029/2024jb029750 article EN Journal of Geophysical Research Solid Earth 2025-01-01

10.1557/jmr.1993.0145 article EN Journal of materials research/Pratt's guide to venture capital sources 1993-01-01

Abstract The absence of reliable paleomagnetic constraints from the Lhasa Block has led to alternative interpretations its late Paleozoic position and timing rifting Gondwana, reflecting uncertainties in early Neo‐Tethyan paleogeography. This study presents geochronological data middle Permian Luobadui Formation, providing a new paleogeographic constraint on Block. Despite possible remagnetization, dual‐polarity magnetization, hosted different minerals lithologies, likely represents...

10.1029/2024gl114347 article EN cc-by-nc Geophysical Research Letters 2025-04-04

Abstract The Clarion and Clipperton Fracture Zones in the Eastern Pacific are well known as a manganese nodule belt, which developed since late Oligocene. slow growth rate of these marine ferromanganese nodules implies that they have potentially recorded long‐term environmental changes. To produce records from nodules, their chronology needs to be established first. In order achieve this objective, many dating methods been applied; however, due relatively low‐resolution temporal constraint,...

10.1029/2019jb018639 article EN Journal of Geophysical Research Solid Earth 2020-06-10

The Lower Cretaceous Dalazi Formation in the Yanji Basin, eastern Jilin Province is of particular interest because it contains key fresh water fossil taxa, oil and gas resources, a potential terrestrial Albian–Cenomanian boundary, regional unconformities. However, lack precise chronology for non-marine strata has precluded better understanding stratigraphic correlation processes. Here, we report magnetostratigraphic U–Pb geochronologic results sedimentary sequence from Xing’antun section...

10.3390/min11050527 article EN Minerals 2021-05-17

Standard-size samples are usually used for traditional paleomagnetic studies. In some cases, small irregular employed considering their amount and magnetic strength as well experiment efficiency. With the development of deep space exploration, demand studying weak is increasing. this study, we established a measurement technique rare samples. We designed low-background, sample-nondestructive high-flexibility holders with various materials different measurements customized holders, estimated...

10.3389/feart.2023.1146231 article EN cc-by Frontiers in Earth Science 2023-03-30

Although epitaxial growth of Si films on both surfaces silicon wafer (epi-Si/Si-wafer/epi-Si) can be realized in foundry by means mounting certain amounts wafers a boat commercial specialized chemical vapor deposition equipment (s-CVD), for its counterpart epi-SiC/Si-wafer/epi-SiC, neither is it readily s-CVD, nor easily achieved conventional (c-CVD) which generally used 3C-SiC single surface (epi-SiC/Si-wafer). Since the epi-SiC/Si-wafer/epi-SiC one run more efficient, and anticipated, this...

10.1149/2.0121701jss article EN cc-by-nc-nd ECS Journal of Solid State Science and Technology 2016-12-14

Seamounts are ubiquitous topographic units in the global oceans, and Caiwei Guyot Magellan of western Pacific is a prime example. In this study, we analyzed well-dated sediment core using magnetic properties, grain size, metal enrichment to uncover regional ventilation history during middle Pleistocene explore potential linkages climate changes. Our principal findings as follows: (1) The median size 3.3 ± 0.2 μm, clay silt particles exhibit minimal variation, with average values 52.8 1.8%...

10.3389/fmars.2024.1470134 article EN cc-by Frontiers in Marine Science 2024-10-11

Understanding sediment dynamics and their controlling factors is essential for Quaternary studies, yet they remain poorly documented in the Mariana Trench. In this work, we examine basic character from a core collected at depth of 6470 m southern part Trench, documenting changes sedimentary over past ~440 kyr. Our primary findings are as follows: (1) The median grain size 13.6 ± 12.0 μm, minimal clay (30.9 9.4%) silt (56.6 4.0%) contents, indicating low-dynamic depositional environment; (2)...

10.3389/fmars.2024.1463564 article EN cc-by Frontiers in Marine Science 2024-11-26
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