Results 11 to 20 of about 115 (106)
Introduction The Bafq mining district (BMD) in the Kashmar-Kerman tectonic zone hosts ~34 magnetite-hematite-apatite ore deposits with about 1500 Mt of reserves in the central Iran (Torab, 2008).
kiamars hosseini +2 more
doaj +1 more source
The eastern Tianshan metallogenic belt is an important molybdenum resource base in Xinjiang and is characterized by large-scale porphyry Mo deposits formed during the Triassic.
Ping Li +7 more
doaj +1 more source
Introduction REE should be evaluated in rocks and minerals due to their behavior in complex geochemical processes leading to their use as tracers in geochemical environments.
Kiamars Hosseini +1 more
doaj +1 more source
Introduction The Lakehsiah mining district is hosted in Early Cambrian volcano-sedimentary units (CVSU) of the Kashmar–Kerman zone, Central Iran. The Kashmar-Kerman belt is located between the Yazd block in the west and the Tabas block in the east and ...
Meisam Gholipoor +3 more
doaj +1 more source
Introduction The lenticular Shahneshin barite deposit (N: 35°39'36'' and E: 46°36'11'') is located 80 km northeast of Marivan, Kurdistan Province; north Sanandaj-Sirjan Zone (Stöcklin, 1968).
Hadi Amin-Rasouli +2 more
doaj +1 more source
The Lower Paleozoic reservoir in the Micangshan tectonic zone is a new shale gas exploration area with excellent potential. However, the hydrocarbon migration and accumulation histories of this reservoir have not been thoroughly elucidated and urgently ...
Tao Tian +6 more
doaj +1 more source
Introduction Extensive Eocene–Oligocene magmatic rocks in the Lut–Sistan region, eastern Iran crop out as a huge magmatic province (Pang et al., 2013).
Fatemeh Yari +2 more
doaj +1 more source
Zebra textures in fault‐controlled, hydrothermal dolomite bodies are polygenetic in origin, involving (I) replacement dolomitization, (II) dilatational fracturing and the precipitation of saddle dolomite as a cement, (III) secondary fracturing and the formation of boxwork textures/dolomite breccias and (IV) recrystallization during the later stages of ...
Cole A. McCormick +6 more
wiley +1 more source
Abstract Fluid inclusion water isotope measurements in speleothems have great potential for paleoclimate studies as they enable the reconstruction of precipitation dynamics and land temperatures. Several previous observations, however, suggest that inclusion waters do not always reflect the isotopic composition of surface precipitation.
A. Fernandez +6 more
wiley +1 more source
Fault controlled dolomitisation within Visean carbonates formed along strike‐slip faults activated by basin inversion during the Variscan Orogeny. Fluids were sourced from adjacent hanging wall basins. As porosity was reduced by dolomitisation, fluids were forced under pressure into fracture splays and en echelon normal faults, leading to brecciation ...
Catherine J. Breislin +6 more
wiley +1 more source

