Results 91 to 100 of about 30,693,449 (167)
We present ID-TIMS U-Pb single zircon ages and major and trace element data for granitoid plutons from the Imorona–Itsindro and Kiangara suites in central Madagascar, in order to constrain the timing of igneous emplacement and investigate the ...
Tsilavo Raharimahefa +2 more
doaj +1 more source
Geology and geochemistry of granitoid rocks in Panggong Lalat, Gua Musang, Kelantan [PDF]
This research focussed on the geology and geochemistry of granitoid rocks in Panggong Lalat , Gua Musang Kelantan. The objectives of the research are to produce the geological map of 1:25000 scales of the study area, determined the petrography and ...
Nur Alia Zulkifli,
core
The concept of suites within granitoid batholiths must be treated with extreme caution, especially when petrogenic interpretation of identified suites is involved (e.g. infrastructural control of granitoid suite composition).
Whitten, E. H.T., E. H. T. Whitten
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The middle Cretaceous granitoid plutons of the Shalair Valley, situated in northeastern Iraq, constitute a principal magmatic component of the Sanandaj–Sirjan Zone within the northwestern segment of the Zagros Orogenic Belt.
Imad Kadhim Abdulzahra +3 more
doaj +1 more source
The Upper Cretaceous Beypazari granitoid of the western Ankara, Turkey, is composed of two different units, on the basis of petrography and geochemical composition; these are granodiorite and diorite. The granitoid is subalkaline, belonging to the high-K
YÜCEL ÖZTÜRK, YEŞİM +6 more
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MINERALOGY AND GEOCHEMISTRY OF BAGINDA HILL GRANITOID, BELITUNG ISLAND, INDONESIA
Granitoid spread outs widely throughout Belitung Island, Indonesia. The distribution of granitoid in northwestern part of Belitung Island is associated with tin deposit.
Ikhsan, Naufal, Titisari, Anastasia Dewi
core
Petrological and geochemical characteristics of the Granitoid complex of astaneh, western Iran, from the point of beneficiation [PDF]
The Granitoid Complex of Astaneh closed to Boroujerd belongs to the Sanandaj-Sirjan Zone (SSZ) in the western of Iran. It is elongated and parallel to the prevailing schistosity in the metamorphic rocks by the trend of NW–SE and consists of quartz ...
Saket, Ali +3 more
core +1 more source
Sr and Nd isotopic characteristics of some S-, I- and A-type granitoids from central Anatolia
: The petrogenesis of some Late Cretaceous S-, I- and A-type granitoids in the Aksaray and Kırflehir regions of Central Anatolia is investigated by means of whole-rock Sr and Nd isotope data with supplementary field, petrographic, and whole-rock ...
Göncüoğlu, Mehmet Cemal +3 more
core
Geochemistry and geochronology of I-type granitoid rocks in the northeastern central Iran plate
The Taknar and Sabzevar Zones in the northeastern Central Iran Plate (CIP) encompass a large variety of volcanic and plutonic rocks. The plutonic rocks are mainly I-type granitoids, ranging in age from Late Jurassic to Middle-Late Eocene.
Abolfazl Soltani (12274652)
core +1 more source

