The thermal regimes of large igneous provinces (LIPs) are addressed in order to evaluate
the principal mechanisms of supercontinent breakup. The primary magma solutions and …

The genesis of large igneous provinces (LIP) is controlled by multiple factors including
anomalous mantle temperatures, the presence of fusible fertile components and volatiles in …

Rationale In situ trace element analysis of melt inclusions by laser ablation inductively
coupled plasma mass spectrometry (LA‐ICP‐MS) provides important geochemistry …

Dichotomous high-Ti and low-Ti magmas are ubiquitous in large igneous provinces (LIPs).
These magmas often form economically critical Fe–Ti oxide ores in layered intrusions via …

Large igneous provinces on Earth result from anomalously enormous volcanic eruptions at
high melt production rates. These eruptions are often linked to catastrophic events such as …

The mechanisms and processes by which subducted slab interacted with mantle plume
remain controversial, as direct observation of such interaction is difficult to impossible …

Identification of the nature of recycling crustal materials in the sources of large igneous
provinces (LIPs) is crucial for understanding compositional heterogeneity of the deep …

The oxygen fugacity (fO 2) of the Earth's mantle is a key parameter that regulates
fundamental geological processes such as planetary differentiation, mantle melting, and …

It is generally believed that the Cenozoic basalts distributed across eastern China, east of
the Daxinganlin-Taihangshan gravity lineament (DTGL), are related to the big mantle wedge …

Abstract High-Ti and low-Ti lava series occur simultaneously in many large igneous
provinces (LIP); however, their origins remain debated. To address this issue, we performed …