Results 41 to 50 of about 48,430 (124)
Abstract Vulcanian eruptions are classically associated with the launch of ballistic ejecta and particularly with the production of breadcrust bombs. Morpho‐textural analysis of these ejecta provides critical insight into the poorly constrained processes controlling the complex dynamics of Vulcanian activity.
P. Gabellini +4 more
wiley +1 more source
Abstract The Gyeonggi Massif is one of the major Precambrian basements in the Korean Peninsula where Paleoproterozoic orthogneiss and paragneiss were widely exposed. In this study, newly identified Rhyacian to Orosirian meta‐igneous rocks from the northwestern Gyeonggi Massif (Soyeonpyeongdo and Ganghwado areas) were investigated to elucidate their ...
Seung Hwan Lee +5 more
wiley +1 more source
Types and genesis of the enclaves in Central Anatolian granitoids
Central Anatolian granitoids range from tonalite-monzonite, through granodiorite, to alkali feldspar granite in composition, and typically have angular to oval-shaped mafic magmatic and metamorphic enclaves.
Güleç, Nilgün Türkan +2 more
core +1 more source
GSA Data Repository Item 2020193, GSA Bulletin. File size: about 3660 KB. Appendix 1: Location of analyzed samples; Appendix 2: (A) Electron microprobe standards and detection limits; (B) Detection limits of whole-rock elemental analyses; Appendix 3 ...
P. Quelhas (9011978), et al. (281964)
core +1 more source
Abstract The East Kunlun Orogen (EKO) on the northern margin of the Tibetan Plateau experienced complex Late Paleozoic–Early Mesozoic tectono‐magmatic activities associated with the subduction and closure of the Paleo‐Tethys Ocean. Controversies remain regarding the timing and processes of the transition from subduction to collision and post‐collision,
Xiaodong Wang +5 more
wiley +1 more source
Geochemistry of microgranular enclaves and host granodiorite from Oledo, Central Portugal [PDF]
Geochemistry of microgranular enclaves and host granodiorite from Oledo, Central ...
Silva, M.M.V.G. +2 more
core +2 more sources
Magmatic structures related to the mechanical interaction between mafic magmas and granitoids have been studied in the Valle Fértil calc-alkaline igneous complex, Argentina.
Martino, Roberto Donato +7 more
core
Abstract 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. Among these plutons, the equigranular Aulan body (AG) and the porphyritic Laladar body (LG) were crystallized at 111.0 ±
Imad Kadhim Abdulzahra +3 more
wiley +1 more source
The granitoid intrusive rocks east of Kuh-Dom, northeast of Ardestan, form part of the Urumieh-Dokhtar Magmatic Arc (UDMA) in central Iran. Their compositions range from granodiorite and quartz monzodiorite to diorite.
Ayat Sotoudeh +2 more
doaj +1 more source
Abstract The closure of the Paleo‐Tethys Ocean was one of the most important global geological events which formed the framework of the East Asian continent during the early Mesozoic. The Longmu Co‐Shuanghu suture zone is considered to record closure of the main basin of the Paleo‐Tethys Ocean.
Jinyong Li +6 more
wiley +1 more source

