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The cratonic crust contains abundant mineral deposits of metals such as gold, copper and rare earths and is underlain by a thick mantle lithosphere rich in the volatiles carbon, sulfur and water. Although volatiles are known to be key components in metallogenesis, how and where they are distributed in the cratonic lithosphere mantle and their role in the initial enrichment of metals have not been sufficiently explored. Here we compile sulfur and copper contents of global cratonic peridotites, identifying sulfide-rich and copper-rich continental roots at depths of 160-190 km at cratonic margins.

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The Malanjkhand chalcopyrite deposit, India's primary copper ore producer, has potential for enhanced flotation performance. This study employs standard flotation experiments using a mechanical cell, integrating a conventional collecting agent with a novel ester-based collector blend. A three-factor, three-level Box-Behnken design systematically evaluated experimental parameters, analysed using ANOVA, cubic plots, response surface methodologies.

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A deeper and hotter Martian core-mantle differentiation inferred from FeO partitioning.

Sci Bull (Beijing)

December 2024

State Key Laboratory of Lithospheric and Environmental Coevolution, University of Science and Technology of China, Hefei 230026, China; Deep Space Exploration Laboratory/School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China.

The core-mantle differentiation process plays a pivotal role in redistributing material on a massive scale, shaping the long-term evolution of rocky planets. Understanding this process is crucial for gaining insights into the accretion and evolution of planets like Mars. However, the details of Mars's core-mantle differentiation remain poorly understood due to limited compositional data for its core and mantle.

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Article Synopsis
  • The study focuses on creating iron ore tailings-blast furnace slag (IOT-BFS)-based geopolymers with adjustable setting times and high compressive strength for civil engineering applications.
  • Key factors influencing the setting time include the content of iron ore tailings, alkali content, liquid-solid ratio, and the modulus of alkaline activators, which were thoroughly analyzed.
  • Results show that adjusting the modulus of the alkaline activator significantly affects the setting time, allowing control from around 3 minutes to 108 minutes, enabling tailored geopolymers for diverse construction needs.
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Lithium isotope evidence for a plumeworld ocean in the aftermath of the Marinoan snowball Earth.

Proc Natl Acad Sci U S A

November 2024

Department of Geosciences, Virginia Tech, Blacksburg, VA 24061.

Article Synopsis
  • The snowball Earth hypothesis suggests that during the Marinoan ice age around 635 million years ago, continental chemical weathering was greatly reduced but then increased afterward.
  • Research conducted on lithium isotope compositions in rock layers from South China shows a distinct trend of decreasing lithium levels as distance from the shore increases, indicating the mixing of meltwater and hypersaline seawater.
  • The findings support the idea that during this period, weak weathering on land and strong reverse weathering on the ocean floor influenced the chemistry of the oceans, aligning with the plumeworld hypothesis.
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