Apatite saturation revisited: new model formulations and applications to igneous rocks [0.03%]
关于磷灰石饱和的新思考：新模型的表述及在火成岩中的应用
Benjamin Z Klein,Othmar Müntener,Jack Gillespie et al.
Benjamin Z Klein et al.
Apatite is the primary phosphate mineral in the Earth's crust and is present in a range of intrusive and extrusive igneous rocks, typically at minor to trace quantities. Similarly, apatite is a stable phase in many equilibrium crystallizati...
Phase equilibria modelling of trace element evolution in arc magmas: implications for petrogenesis and copper porphyry indicators [0.03%]
弧火山岩中微量元素演化相平衡模型及其岩浆成因和斑岩铜矿指示意义
Caroline R Soderman,Owen M Weller
Caroline R Soderman
Trace element ratios in arc magmas are widely used to infer petrogenetic conditions, particularly those associated with porphyry-forming versus barren systems. However, quantitatively linking whole-rock signatures to pressure, water content...
Linking crystal shape and dynamic undercooling: a new framework for inferring magmatic crystallization histories [0.03%]
晶体内形与动态过冷之间的联系：推断岩浆结晶历史的新框架
Amanda Lindoo,Madeleine C S Humphreys,Charlotte Gordon et al.
Amanda Lindoo et al.
Magmas contain crystals exhibiting diverse shapes and sizes, yet the relationship between crystal shape (specifically aspect ratio) and undercooling ([Formula: see text]), the driving force for crystallization, remains poorly constrained. C...
Melt reactions and timescales of melting in pelitic rocks-a case study from the Garhwal Himalaya [0.03%]
片岩熔融的熔融反应和熔融时间尺度——来自喜马拉雅加尔瓦尔地区的案例研究
C J Oldman,C J Warren,N B W Harris et al.
C J Oldman et al.
The nature, location, longevity and pressure-temperature conditions of different crustal melt reactions during orogenesis provide constraints on the structure, mechanical strength and exhumation of orogenic middle crust as well as element m...
Coupling antigorite deformation and dehydration in high-pressure experiments [0.03%]
高压实验中抗滑石变形与脱水的耦合机制研究
Lisa Eberhard,Mattia Luca Mazzucchelli,Stefan Markus Schmalholz et al.
Lisa Eberhard et al.
The dehydration of antigorite is an important reaction in subduction zones with implications on both geochemical and geophysical processes. In this experimental study we focus on the onset of antigorite dehydration and investigate various c...
Cooling rates and melt extraction timescales determined by diffusion chronometry on shallow crustal plutonic rocks [0.03%]
浅地壳 plutonic 岩石的冷却速率和熔体萃取时间尺度的扩散定时法确定
Thomas Grocolas,Othmar Müntener,Elias M Bloch et al.
Thomas Grocolas et al.
Diffusion chronometry has emerged as a valuable tool to track the timescales of magmatic processes and is now routinely applied on erupted volcanic products to infer crystal residence times and mixing-to-eruption timescales. Despite some at...
Sabastien C Dyer,Ivan Edgeworth,Brian Kendall et al.
Sabastien C Dyer et al.
Metamorphic zircon is commonly assumed to record growth during prograde or peak metamorphic conditions. However, numerical models of zircon predict growth during cooling. Linking the relative timing of zircon growth to a metamorphic evoluti...
Controls of focused fluid release in subduction zones: insights from experimental dehydration of brucite vein networks in serpentinite [0.03%]
俯冲带富集流体释放的控制：蛇纹岩中纤绿翠石脉网络脱水实验的启示
Manuel D Menzel,Lisa Eberhard,Austin Arias et al.
Manuel D Menzel et al.
Aqueous fluids released by metamorphic dehydration of serpentinites are a key component for seismicity, creep, and geochemical cycling in subduction zones. How these fluids drain and migrate towards the mantle wedge has yet to be fully unde...
Coherent solvus of disordered alkali feldspar: experiment, atom probe tomography and thermodynamic model [0.03%]
无序斜长石的相干溶解度：实验、原子探针层析和热力学模型
D Heuser,R Dubosq,E Petrishcheva et al.
D Heuser et al.
At temperatures above about 600 °C, alkali feldspar forms a continuous solid solution between the Na and K end members. Towards lower temperatures a miscibility gap opens, and alkali feldspar of intermediate composition exsolves, forming a...
Edgar Dachs,Artur Benisek
Edgar Dachs
A new activity model for biotite is formulated in the system K2O-FeO-MgO-Al2O3-SiO2-H2O-TiO2-O2 (KFMASHTO), which extends that for the KFMASH system by introducing a titanium-biotite and a ferric-biotite end-member (tbio: K(TiMg2)[(O)2(AlSi...