Lanterman Range

Di Vincenzo G., Ghiribelli B., Giorgetti G., and Pahneri R. (2001) Evidence of a close link between petrology and isotope records constraints from SEM, EMP, TEM and in situ Ar-40-Ar-39 laser analyses on multiple generations of white micas (Lanterman Range, Antarctica). Earth Planet. Sci. Lett. 192(3), 389-405. 

Lanterman Range, Antarctica Coesite in garnet from eclogite T- 850 °C E >29 kb 500 Ma Ghiribelli et al. (2002)... 

GhiribeUi B., Frezzotti M.-L., and Palmeri R. (2002) Coesite in eclogites of the Lanterman range (Antarctica) evidence from textural and Raman studies. Euro. J. Mineral. 14, 355-360. 

The K-Ar dates of the Wilson Gneisses of the Lanterman Range in Appendix 4.8.3.12 and in Fig. 4.18 indicate that biotite, muscovite, and hornblende reached their blocking temperature for radiogenic Ar... 

The Salamander Range is located southeast of the Lanterman Range and is separated from the Freyberg Mountains by the upper Canham Glacier. The northern part of the Salamander Range consists of Wilson Gneisses which, in the southernmost part, is overlain by residual outcrops of the Beacon Supergroup and of the Kirkpatrick Basalt. 

The rocks of the Bowers Supergroup are locally overlain by erosional remnants of the Beacon Supergroup (Permian to Triassic) which includes sills of the Ferrar Dolerite (Middle Jurassic). In addition, erosional remnants of the Kirkpatrick Basalt plateau (Middle Jurassic) are present adjacent to the Lanterman Range and in the Leitch Massif (Gair et al. 1969). 

Age Determinations of Basement Rocks of the Lazarev Mountains, Danieis, Morozumi, and Lanterman Ranges, Wiison Terrane ... 

Capponi G, Crispini L, Meccheri M (1999) Structural history and tectonic evolution of the boundary between the Wilson and Bowers terranes, Lanterman Range, northern Victoria Land, Antarctica. Tectonophysics 312 249-266... 

DiVincenzo G, Palmeri R, Talaiico F, Andiiesen PAM, Ricci C (1997) Petrology and geochronology of eclogites from the Lanterman Range, Antarctica J Petrol 38 1391-1417... 

The unnamed glacial diamictite occurs in a down-faulted block of the western Lanterman Range in Fig. 10.12. It is about 250 m thick (McKelvey 1983 ... 

McKelvey BC (1983) A palaeogeographic comparison of the late Palaeozoic Lanterman Range tiUite of northern Victoria Land, Antarctica, with equivalent tillites in eastern AustraUa. Geol Soc Amer, Abstracts with Programs 15(4) 215... 

---