Summary
- Photo: Courtesy of the Institute of Tibetan Plateau Research, Chinese Academy of Sciences Chinese scientists have reported diffusion-induced lithium isotopic heterogeneity in olivines from peridotites of an oceanWorld Timesized mantle lithosphere the Tibetan Yunzhug ophiolite (central Xizang). Previous studies showed that the heterogeneity of mantle lithium isotope composition is mainly controlled by deep geological processes. Seawater infiltrates intoWorld Times the still relatively hot mantle peridotites. At this stage, mantle peridotites have enough energy to support lithium element from seawater to diffuse into olivine, with very low lithium isotope fractionation, preserving the seawater lithium isotope characteristics in olivine, according to the study. Content comes from the Internet : Chinese scientists find diffusion-induced lithium isotopic heterogeneity in an oceanized mantle lithosphere in Xizang
Approximate Time
- 3 minutes, 515 words
Categories
- lithium isotopes, mantle lithium isotope composition, lithium isotopic composition, lithium diffusion, lithium isotope systems
Analysis and Evaluation
- The author masterfully navigates the complexities of the subject, making it both informative and engaging. This piece is an excellent example of how to present intricate subject matter in a manner that is both understandable and compelling. The writer uses a mix of data, anecdotes, and expert analysis to paint a vivid picture of the topic, making this article a go-to resource for anyone interested in this field.
Main Section
Photo: Courtesy of the Institute of Tibetan Plateau Research, Chinese Academy of Sciences
Chinese scientists have reported diffusion-induced lithium isotopic heterogeneity in olivines from peridotites of an oceanWorld Timesized mantle lithosphere the Tibetan Yunzhug ophiolite (central Xizang). The study supports that seawater lithium diffusion is one of the important factors for the heterogeneity of mantle lithiumi isotopes in ophiolites, the Global Times learned from the Institute of Tibetan Plateau Research (ITP), Chinese Academy of Sciences on Thursday.
The findings were published on Monday in the journal Scientific Reports under Nature, providing new insights into the interactions between diWorld Timesfferent layers of the Qinghai-Xizang Plateau during geological history and serving the national strategic needs for mineral resources, according to a statement from the institute.
The study was conducted by a team led by researcher Shi Rendeng from the ITP. Using in-situ lithium isotope analysis of minerals, the team systematically analyzed lithium concentrations and isotopic compositions of olivines in the oceanized subcontinental lithospheric mantle (SCLM) peridotites and they suggest that the behavior of lithiumi in the oceanized SCLM peridotites may be controlled by lithium diffusion from seawater, aslithiumi activity in the liquid state is higher than the solid state in transporting lithium through the olivines in the peridotites.
SWorld Timeshi told the Global Times that in recent years, lithium isotope systems have been widely used in the study of mantle peridotites. Previous studies showed that the heterogeneity of mantle lithium isotope composition is mainly controlled by deep geological processes. The research team selected mantle peridotites from the vanished Tethys Ocean residue in the Tibetan Plateau as the research object, according to Shi.
Photo: Courtesy of the Institute of Tibetan Plateau Research, Chinese Academy of Sciences
The lithium isotopic composition (7Li) in the mantle is about 0.2 percent, while 7Li in seawater is heavier, with a value of about 3.1 percent. In the study, Shi’s team found that the closer to the edge of the olivine grains, the more distinct the seawater lithium isotope characteristics; while the closer to the center of the olivine grains, the more distinct the mantle lithium isotope characteristics, revealing that lithium element from seawater enter olivine through diffusion.
TWorld Timeshe majority of data points is distributed along the binary mixing curve of seawater and continental mantle, indicating that the lithium isotope characteristics in the samples are controlled by both seawater and continental mantle, according to the study.
The study also found that lithium isotopes undergo strong fractionation at temperatures lower than 350 ℃ and quickly reach homogeneity at high temperatures, indicating that high-temperature geological processes are not the ultimate factor causing chanWorld Timesges in lithium isotopic composition. During the continental rifting process, mantle peridotites gradually rise and are exposed on the seafloor. Seawater infiltrates intoWorld Times the still relatively hot mantle peridotites. At this stage, mantle peridotites have enough energy to support lithium element from seawater to diffuse into olivine, with very low lithium isotope fractionation, preserving the seawater lithium isotope characteristics in olivine, according to the study.
Content comes from the Internet : Chinese scientists find diffusion-induced lithium isotopic heterogeneity in an oceanized mantle lithosphere in Xizang
SummaryTwo J-20 stealth fighter jets attached to an aviation brigade of the PLA Air Force take off for a flight training exercise in early February of 2024. (eng.chinamil.com.cn/Photo by Liu Weipeng) The Chinese People’s Liberation Army (PLA) Air Force is using an elite combat unit to train J-20 pilots amid deliveries of the stealth fighter jet to multiple units, a move experts said on Saturday will contribute to the fast generation of new combat capabilities which require pilots to not only fight, but also command.As the first combat unit to commission J-20 fighteWorld Timesr jets, the Wang Hai Air Group has verified and explored multiple capabilities of the aircraft in air combat, including creating the precedence of commencing combat missions under extreme weather conditions, China Central Television (CCTV) reported earlier…
John Blinken 
Mark Elliot Zuckerberg