Results 31 to 40 of about 5,853 (215)

A mountain slope deformation in an alpine metaophiolitic massif (Ligurian Alps, Italy)

Journal of Maps, 2021
Deep-seated gravitational slope deformation (DsGSD) represents a relevant geological-geomorphological feature of the landscape and has drawn scientific attention for the past several decades.
F. Faccini, L. Federico, S. Torchio, A. Roccati, G. Capponi, L. Crispini   +5 more
doaj   +1 more source

Geology and Petrology of Southeast Albanian Ophiolites

, 2022
The ophiolitic complexes of southeastern Albania (Shpat-Kuterman Massif, Shebenik-Pogradec, Devoll, Vallamare, Voskopoja, Morava, Vithkuq-Rehova and the ultrabasic outcrops of Bitincke-Kapshtica) are represented by the Lercolite, Gabritolite, Kharchian ...
Friedrich Koller, Gjon Rrota, Kujtim Onuzi, Gjon Kaza   +3 more
core   +1 more source

MAGMATIC ROCKS OF THE TEKTURMASS ACCRETIONARY COMPLEX, CENTRAL KAZAKHSTAN: GEOLOGICAL POSITION AND GEODYNAMIC SETTINGS OF FORMATION

Геодинамика и тектонофизика, 2022
The paper provides an overview of the geological structure and presents new data on petrography and geochemistry of igneous rocks of the Tekturmas accretionary complex (TAC).
A. V. Gurova, I. Yu. Safonova, I. A. Savinsky, R. M. Antonyuk, T. Zh. Orynbek   +4 more
doaj   +1 more source

Ophiolites of Iran : keys to understanding the tectonic evolution of SW Asia : (II) Mesozoic ophiolites

, 2015
Iran is a mosaic of continental terranes of Cadomian (520-600 Ma) age, stitched together along sutures decorated by Paleozoic and Mesozoic ophiolites. Here we present the current understanding of the Mesozoic (and rare Cenozoic) ophiolites of Iran for ...
Stern, Robert J, Moghadam, Hadi Shafaii
core   +1 more source

Carboniferous and Permian evolutionary records for the Paleo-Tethys Ocean constrained by newly discovered Xiangtaohu ophiolites from central Qiangtang, central

, 2016
Reconstructing the evolutionary history of the Paleo-Tethys Ocean remains at the center of debates over the linkage between Gondwana dispersion and Asian accretion.
Xia, Xiao-Ping, Liang, He, Xu, Wang, Zhang, Xiu-Zheng, Zhang, Chunfu, Dong, Yong-Sheng, Wang, Qiang, Dan, Wei, Deng, Ming-Rong, Zeng, Ji-Peng   +9 more
core   +1 more source

Tectono-metamorphic and magmatic evolution of the Internal Dinarides (Kopaonik area, southern Serbia) and its significance for the geodynamic evolution of the Balkan Peninsula [PDF]

, 2012
The study is devoted to the tectono-metamorphic and magmatic evolution of the Internal Dinarides and it furthermore addresses the geodynamic evolution of the Balkan Peninsula.
Schefer, Senecio
core   +1 more source

Petrogenesis and tectonic setting of the Yushishan and Yueyashan ophiolites in the Beishan orogenic belt, China: constraints on the evolution of the southern margin of the middle Paleo-Asian Ocean in early cambrian

Frontiers in Earth Science
The occurrence of ophiolites in the Beishan Orogenic Belt (BOB), located in the southern Central Asian Orogenic Belt (CAOB), is critical for elucidating the tectonic evolution of the southern part of the Paleo-Asian Ocean (PAO).
Lei Wu, Lei Wu, Xinwei Zhai, Xinwei Zhai, Yuxi Wang, Yuxi Wang, Qingqing Yin, ShuYu Jin, Xinrong Liu, Guoxin Zhang, Erteng Wang, Kai Yu, Jinrong Wang, Xiao Tian, Xiao Tian, Ju Wang, Ju Wang, Xia Li   +17 more
doaj   +1 more source

Geology of the eastern part of the Tso Morari nappe, the Nidar Ophiolite and the surrounding tectonic units (NW Himalaya, India)

Journal of Maps, 2019
The Tso Morari nappe is well known for having suffered ultrahigh-pressure metamorphism in the northwest Himalaya. Its pressure-temperature evolution has been widely studied and debated since the end of the 1990s.
Nicolas Buchs, Jean-Luc Epard
doaj   +1 more source

GEOCHEMISTRY AND ORIGIN OF THE EASTERN SAYAN OPHIOLITES, TUVA-MONGOLIAN MICROCONTINENT (SOUTHERN SIBERIA) [PDF]

, 2017
The Eastern Sayan ophiolites (1020 Ma) of the Tuva-Mongolian microcontinent are believed to be the most ancient ophiolite of the Central Asian Orogenic Belt [Khain et al., 2002].The Eastern Sayan ophiolites (1020 Ma) of the Tuva-Mongolian microcontinent ...
M. A. Gornova, Yu. V. Noskova, K.-L. Wang, A. A. Karimov, A. Ya. Medvedev, V. A. Belyaev, S. I. Dril’   +6 more
core   +1 more source

Mesostructural paragenesises of the southeastern part of the Ebeta antiform (Northern Kazakhstan)

Известия высших учебных заведений: Геология и разведка, 2015
Data on a geoiogical structure and evolution of mesostructural complexes of a southeast part of the Ebeta antiformhas been provided. Multistage nature of the deformations and a metamorphism of a Mamyt metamorphic complex and its frame have been ...
B. G. Golionko, O. A. Artemova
doaj   +1 more source