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and 96P4e resemble high-K, peraluminous S-type granitoids (Fig. 3.5b-c). Rb-mobility
may cause a transitional position between volcanic arc and collision-related tectonic
setting (Fig. 3.5f-i). The rock samples show different degrees of REE enrichment with
La N/Lu N = 16.7 (L96M25a), 13.0 (96P4e), and 7.8 (L96A9) (Fig. 3.6c).
The Cretaceous monzogranites from the Central Pamirs, RPZ and northernmost South
Pamirs are all high-K, highly peraluminous S-type intrusions. There is some diversity in
this group, probably due to some element mobility of K and Rb. Nevertheless, some
samples are petrologically identified as S-type monzogranites (e.g. the two mica
granite P7). The subalkaline to alkaline subvolcanic latite-andesite A96S1b has a
metaluminous character (Fig. 3.5a-c). The tectonic classification is heterogeneous from
volcanic arc to collisional setting (Fig. 3.5f-i). In chondrite-normalised REE abundance
diagrams all samples show a concave-upward pattern with the highest La N/Lu N values
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