Petrogenetic constraints on the origin and formation of the Hellenic Triassic rift-related lavas
P Koutsovitis, A Magganas, T Ntaflos, N Koukouzas… - Lithos, 2020 - Elsevier
Triassic rift-related volcanic rocks outcrop over all mainland Greece, comprising of
trachybasalts and basaltic trachyandesites. Relatively immobile to the effects of alteration …
trachybasalts and basaltic trachyandesites. Relatively immobile to the effects of alteration …
[HTML][HTML] 岩浆岩中磷灰石的地球化学特征及应用
李子木， 令狐苗苗， 孙金凤， 孙之晗， 周宝全， 杨进辉 - 岩石学报, 2025 - dzkx.org
不同类型的岩浆岩可能来源于不同源区, 经历复杂的岩浆演化过程, 导致岩浆成分,
温度和压力等条件发生变化. 磷灰石在岩浆岩中广泛发育, 可以形成于不同的岩浆环境 …
温度和压力等条件发生变化. 磷灰石在岩浆岩中广泛发育, 可以形成于不同的岩浆环境 …
The Twihinate carbonatite (Moroccan Sahara): Evidence for compositional mantle heterogeneity and northwestern African plate geodynamics
Abstract The Cretaceous Twihinate carbonatite in the Moroccan Sahara is a∼ 5 km
diameter ring-shaped intrusion made of an inner core preserving sparse occurrences of …
diameter ring-shaped intrusion made of an inner core preserving sparse occurrences of …
Monazite and zircon U–(Th–) Pb dating reveals multiple episodes of HT metamorphism in the Cima Lunga unit (Central Alps): implications for the exhumation of high …
High-to ultrahigh-pressure (HP–UHP) rocks recording high-temperature (HT)> 700° C are
well exposed in the Central Alps, making it an ideal region to study the timing of …
well exposed in the Central Alps, making it an ideal region to study the timing of …
Metacarbonatite rocks from Amesmessa area (In Ouzzal Terrane), Hoggar shield, Algeria
M Cherbal, K Yonezu, DE Aissa, T Tindell… - Journal of African Earth …, 2019 - Elsevier
Abstract The Hoggar Shield (South Algeria) belongs to the 3,000 km-long Pan-African Trans-
Saharan Belt which formed in the Neoproterozoic and Cambrian, between 750 and 545 Ma …
Saharan Belt which formed in the Neoproterozoic and Cambrian, between 750 and 545 Ma …
[HTML][HTML] Birth and closure of the Kallipetra Basin: Late Cretaceous reworking of the Jurassic Pelagonian–Axios/Vardar contact (northern Greece)
Abstract Some 20 Myr after the Late Jurassic to Early Cretaceous obduction and collision at
the eastern margin of Adria, the eroded Pelagonia (Adria)–Axios/Vardar (oceanic complex) …
the eastern margin of Adria, the eroded Pelagonia (Adria)–Axios/Vardar (oceanic complex) …