Intensified Continental Weathering and Reductive Surface Runoff During the Triassic–Jurassic Transition

Study on Continental Weathering and Reductive Surface Runoff During the Triassic-Jurassic Transition Academic Background The Triassic-Jurassic Transition (TJT) marks one of the most significant mass extinction events in Earth’s history, known as the End-Triassic Extinction (ETE). This event led to a widespread decline in biodiversity across both ma...

Hidden Deep Sulfide Cumulates Beneath the Jinchuan Ni–Cu–Platinum-Group Element Deposit (China) Inferred from Ni–Cu Isotopes

Discovery of Deep Sulfide Cumulates Beneath the Jinchuan Ni-Cu-Platinum Group Element Deposit and Its Significance Background Introduction Nickel (Ni), copper (Cu), and platinum group elements (PGE) are critical metal resources on Earth, widely used in industries, electronics, and new energy sectors. Approximately 56% of the world’s nickel, 3% of c...

Late Triassic Continental Eclogite in the Central Tibetan Plateau Reveals 2500-km-long Paleo-Tethys Continental Subduction

Late Triassic Continental Eclogite in the Central Tibetan Plateau Reveals Paleo-Tethys Continental Subduction Academic Background The Tibetan Plateau is one of the youngest and highest plateaus on Earth, and its formation is closely related to the closure of the Tethys Ocean and the collision of the Indian-Eurasian plates. The Paleo-Tethys Ocean wa...

Alkali-Carbonate Melts in the Cratonic Mantle Evidenced by a Wehrlite Xenolith from the Majuagaa Kimberlite, West Greenland

Evidence of Alkali-Carbonate Melts in the Mantle Academic Background Carbonate melts play a crucial role in Earth’s deep carbon cycle, mantle melting, redox reactions, and the transport of highly incompatible elements. Although experimental studies, metasomatic transformations, and melt/fluid inclusions in mantle xenoliths, kimberlites, and diamond...

First Dating of an Early Chibanian (Middle Pleistocene) Glacial Overdeepening in the Alpine Foreland Using the 4He/U-Th Method

First Dating of an Early Chibanian (Middle Pleistocene) Glacial Overdeepening in the Alpine Foreland Using the 4He/U-Th Method

First Dating of an Early Chibanian (Middle Pleistocene) Glacial Overdeepening in the Alpine Foreland Using the 4He/U-Th Method Academic Background Glacial overdeepenings are deep valleys formed by glacial erosion, typically filled with glacial sediments. These sediments record the history of glacial activity and are crucial for understanding the ex...