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Tab. 1+2: Representative electron-microprobe analyses of minerals from Du Toi...
An example of cordierite-bearing gneiss that is part of a high-grade gneiss-migmatite sequence is described from the Hatch Plain in the Read Mountains of the Shackleton Range,... -
Tab. 1: Rb-Sr data on metasediments in the Shackleton Range
Summary: The stratigraphy of the Shackleton Range established by Stephenson (1966) and Clarkson (1972) was revised by results of the German Expedition GEISHA 1987/88. The... -
Table A1 LA-ICP-MS zircon U-Pb data of Laoniushan granitoids
The NWW-striking Qinling Orogen formed in the Triassic by collision between the North China and Yangtze Cratons. Triassic granitoid intrusions, mostly middle- to high-K,... -
Tab. 1: Mineralogical composition and chemical analyses of major and trace el...
As a result of a petrographical, mineralogical and geochemical characterization of the Ameghino Formation mudstones (Upper Jurassic- Lower Cretaceous, Antarctic Peninsula),... -
Table 1: U-Pb analyses of zircons and monazites of paragneisses which belong ...
Samples of high grade metamorphic basement rocks of Wilson Terrane cropping out in the Deep Freeze Range and on Kay Island were collected during GANOVEX VI to study their... -
Tab. 2: U-Pb ion-microprobe ages from Taymyr peninsula
We present the initial results of a U-Th-Pb zircon ion-microprobe investigation on samples from the Central Belt of Taimyr, in order to constrain its tectono-magmatic evolution.... -
Tab. 1: Trace-element concentrations in ore samples collected from mercury mi...
A belt of small but numerous mercury deposits extends for about 500 km in the Kuskokwim River region of southwestern Alaska. The southwestern Alaska mercury belt is part of... -
Tab.1: Composition of salt crusts and host rocks
Gypsum and calcite crusts were found on many outcrops of the metamorphic basement and on moraines in Dronning Maud Land. For the first time the copper mineral connellite was... -
Tab.1: Representative bulk-rock and trace element chemistry
High-pressure/low-temperature metabasites occupy a definite geological position within the structure of the Polar Urals and have a very important bearing on the understanding of... -
Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula
Morphological and U-Pb isotope studies on sedimentary zircons reflect the orogenic evolution of their former host rocks. The orogenic history of detrital zircons from the... -
Tab. 1: U-Pb analyses of zircons from rock samples in MT. Newton and Cumpston...
We present new U-Pb zircon (SHRIMP) data on rocks from Mt Newton and Cumpston Massif in the southern Prince Charles Mountains. Our data demonstrate that Mt Newton was affected... -
Electron microprobe results of clay minerals from samples of the Frankenwald ...
Late Devonian (Frasnian) pillow basalts from the Frankenwald and Thüringer Wald within the Saxothuringian zone in Germany were found to contain abundant putative biogenic... -
Tab. 1: Proportion of glacial quartz grains contained in the deposits
The Yari-Hotaka Mountain Range is one of the most famous formerly-glaciated areas of Japan. Many glacial landforms remain in three neighbouring U-shaped valleys, named Yarisawa,... -
Tab. 1+2: C14-dates cf the older and younger emergence periods
In the neighbourhood of Oobloyah Bay various phenomena ean be eneountered whieh point to a ularge-seale uplift of shorelines, i.e. to an emergence of 200 m. Delta terraces,... -
Tab. 1: Ar40/Ar39 results from Kuyul terrane, northeastern Russia
The Kamchatka Peninsula of northeastern Russia is located along the northwestern margin of the Bering Sea and consists of zones of complexly deformed accreted terranes. Along... -
(Table 3) K-Ar dating of trachybasalts from the Sinii Utes Depression, Southe...
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