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Thermal Constraints on the Emplacement Rate of a Large Intrusive Complex: The Manaslu Leucogranite, Nepal Himalaya

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Academic year: 2021

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Figure

Fig. 1. Generalized geological map of the Manaslu area in central Nepal, after Colchen et al
Fig. 2. P–T diagram showing the locations of the main dehydration melting reactions (MS, muscovite schist and MBS, muscovite–biotite schist) involving muscovite, obtained for two Himalayan metapelites by Patin˜o Douce & Harris (1998), together with the
Fig. 3. One-dimensional model of emplacement of a large igneous body by discrete sill accretion
Fig. 4. Equilibrium temperature T i at the HHC–sediment interface for different sediment conductivities k se and HHC conductivities k sl
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