[HTML][HTML] Layered intrusions: Fundamentals, novel observations and concepts, and controversial issues

RM Latypov, O Namur, Y Bai, SJ Barnes… - Earth-Science …, 2024 - Elsevier
Layered intrusions are fossilized natural laboratories that historically have constrained many
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …

[HTML][HTML] Two stages of immiscible liquid separation in the formation of Panzhihua-type Fe-Ti-V oxide deposits, SW China

MF Zhou, WT Chen, CY Wang, SA Prevec, PP Liu… - Geoscience …, 2013 - Elsevier
Magmatic oxide deposits in the∼ 260 Ma Emeishan Large Igneous Province (ELIP), SW
China and northern Vietnam, are important sources of Fe, Ti and V. Some giant magmatic Fe …

[HTML][HTML] The Emeishan large igneous province: A synthesis

JG Shellnutt - Geoscience Frontiers, 2014 - Elsevier
Abstract The late Permian Emeishan large igneous province (ELIP) covers∼ 0.3× 10 6 km 2
of the western margin of the Yangtze Block and Tibetan Plateau with displaced, correlative …

Fe–Ti–V–P ore deposits associated with Proterozoic massif-type anorthosites and related rocks

B Charlier, O Namur, O Bolle, R Latypov… - Earth-Science …, 2015 - Elsevier
Magmatic rocks containing economic concentrations of iron, titanium, vanadium and
phosphorous are commonly associated with massif-type anorthosites and related rocks. This …

A review of magnetite geochemistry of Chilean iron oxide-apatite (IOA) deposits and its implications for ore-forming processes

G Palma, F Barra, M Reich, AC Simon, R Romero - Ore Geology Reviews, 2020 - Elsevier
Magnetite is the most important iron ore in iron oxide-apatite (IOA) deposits which represent
the Cu-poor end-member of the iron oxide-copper–gold (IOCG) clan. Magnetite chemistry …

Whole-rock and mineral composition constraints on the genesis of the giant Hongge Fe-Ti-V oxide deposit in the Emeishan Large Igneous Province, Southwest China

ZJ Bai, H Zhong, AJ Naldrett, WG Zhu… - Economic …, 2012 - pubs.geoscienceworld.org
Abstract The Hongge giant Fe-Ti-V oxide ore deposit is hosted by a layered intrusion located
in the central part of the Emeishan large igneous province, SW China. The intrusion is …

Experimental study of high-Ti and low-Ti basalts: liquid lines of descent and silicate liquid immiscibility in large igneous provinces

Y Zhang, O Namur, B Charlier - Contributions to Mineralogy and Petrology, 2023 - Springer
Dichotomous high-Ti and low-Ti magmas are ubiquitous in large igneous provinces (LIPs).
These magmas often form economically critical Fe–Ti oxide ores in layered intrusions via …

Mineralogy and origin of exsolution in Ti-rich magnetite from different magmatic Fe-Ti oxide-bearing intrusions

W Tan, P Liu, H He, CY Wang… - The Canadian …, 2016 - pubs.geoscienceworld.org
Titanium-rich magnetite from different magmatic Fe-Ti oxide-bearing intrusions consists of
host magnetite (nearly pure Fe3O4) and different types of exsolution. The exsolution of Ti …

New textural and mineralogical constraints on the origin of the Hongge Fe-Ti-V oxide deposit, SW China

CY Wang, MF Zhou - Mineralium Deposita, 2013 - Springer
Abstract The Hongge magmatic Fe-Ti-V oxide deposit in the Panxi region, SW China, is
hosted in a layered mafic–ultramafic intrusion. This 2.7-km-thick, lopolith-like intrusion …

Experimental Constraints on the Storage Conditions and Differentiation of High-Ti Basalts from the Panzhihua and Hongge Layered Intrusions, SW China

D Wang, T Hou, R Botcharnikov… - Journal of …, 2024 - academic.oup.com
High-Ti basalts are commonly believed to represent parental magmas leading to the
formation of mafic-ultramafic layered intrusions, such as Late Permian Panzhihua and …