Lithosphere Q2
Unclaimed
Lithosphere is a journal indexed in SJR in Geology with an H index of 61. It is an CC BY Journal with a Double blind peer review review system The scope of the journal is focused on solid Earth, geochemistry, geodynamics, geochronology, geoanalytical techniques, lithogenesis. It has an SJR impact factor of 0,455 and it has a best quartile of Q2. It is published in English, Russian. It has an SJR impact factor of 0,455.
Type: Journal
Type of Copyright: CC BY
Languages: English, Russian
Open Access Policy: Open Access
Type of publications:
Publication frecuency: -
- €
Inmediate OANPD
Embargoed OA- €
Non OAMetrics
0,455
SJR Impact factor61
H Index91
Total Docs (Last Year)477
Total Docs (3 years)6033
Total Refs876
Total Cites (3 years)476
Citable Docs (3 years)1.84
Cites/Doc (2 years)66.3
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Aims and Scope
Best articles by citations
Gneiss domes, vertical and horizontal mass transfer, and the initiation of extension in the hot lower-crustal root of a continental arc, Fiordland, New Zealand
View moreTowards a clarification of the provenance of Cenozoic sediments in the northern Qaidam Basin
View moreAn orogenic wedge model for diachronous deformation, metamorphism, and exhumation in the hinterland of the northern Canadian Cordillera
View moreA survey of Sierra Nevada magmatism using Great Valley detrital zircon trace-element geochemistry: View from the forearc
View moreLate Triassic tectonic framework and evolution of Central Qiangtang, Tibet, SW China
View moreDetrital geochronology of pre-Mississippian strata in the northeastern Brooks Range, Alaska: Insights into the tectonic evolution of northern Laurentia
View moreForeland-directed propagation of high-grade tectonism in the deep roots of a Paleoproterozoic collisional orogen, SW Montana, USA
View moreCooling and exhumation along the curved Albany-Fraser orogen, Western Australia
View moreNew biostratigraphic evidence of Late Permian to Late Triassic deposits from Central Tibet and their paleogeographic implications
View moreRift- and subduction-related crustal sequences in the Jinshajiang ophiolitic melange, SW China: Insights into the eastern Paleo-Tethys
View moreTiming and rates of Holocene normal faulting along the Black Mountains fault zone, Death Valley, USA
View moreAges and geochemistry of Early Jurassic granitoids in the Lesser Xing'an-Zhangguangcai Ranges, NE China: Petrogenesis and tectonic implications
View moreDetrital zircon record of mid-Paleozoic convergent margin activity in the northern U.S. Rocky Mountains: Implications for the Antler orogeny and early evolution of the North American Cordillera
View moreDetrital zircon U-Pb geochronology of the Sierra de Santa Rosa Formation, Sonora, Mexico, and implications for an Early Jurassic retroarc basin
View moreDetrital zircons from Cretaceous midcontinent strata reveal an Appalachian Mountains-Cordilleran foreland basin connection
View moreMantle flow at the highly arcuate northeast corner of the Lesser Antilles subduction zone: Constraints from shear-wave splitting analyses
View moreCrustal growth and tectonic evolution of the Mojave crustal province: Insights from hafnium isotope systematics in zircons
View moreA Jurassic oceanic core complex in the high-pressure Monviso ophiolite (western Alps, NW Italy)
View moreCretaceous partial melting, deformation, and exhumation of the Potters Pond migmatite domain, west-central Idaho
View moreCrustal melting, ductile flow, and deformation in mountain belts: Cause and effect relationships
View morePunctuated shortening and subsidence in the Altiplano Plateau of southern Peru: Implications for early Andean mountain building
View moreQuantifying rates of "rifting while drifting" in the southern Gulf of California: The role of the southern Baja California microplate and its eastern boundary zone
View moreConstraining the timing of shale detachment faulting: A geochemical approach
View moreSlip rate and recurrence intervals of the east Lenglongling fault constrained by morphotectonics: Tectonic implications for the northeastern Tibetan Plateau
View more
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