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NARROW
GeoRef Subject
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Jordan
Well performance in relation to design, construction and wellfield operation: a case study from the fossil Ram Sandstone aquifer in southern Jordan
Deynekoite, Ca 9 □Fe 3+ (PO 4 ) 7 – a new mineral of the merrillite group from phosphide-bearing contact facies of paralava, Hatrurim Complex, Daba-Siwaqa, Jordan
Rock mechanical properties of immature, organic-rich source rocks and their relationships to rock composition and lithofacies
Nickolayite, FeMoP, a new natural molybdenum phosphide
Miocene to sub-Recent magmatism at the intersection between the Dead Sea Transform and the Ash Shaam volcanic field: evidence from the Yarmouk River gorge and vicinity
Natural and Anthropogenic Analogues for High-Level Nuclear Waste Disposal Repositories: A Review
Priscillagrewite-(Y), (Ca 2 Y)Zr 2 Al 3 O 12 : A new garnet of the bitikleite group from the Daba-Siwaqa area, the Hatrurim Complex, Jordan
Mcconnellite, CuCrO 2 and ellinaite, CaCr 2 O 4 , from varicoloured spurrite marble of the Daba-Siwaqa area, Hatrurim Complex, Jordan
Liquefaction susceptibility maps for the Aqaba–Elat region with projections of future hazards with sea-level rise
Stress in the tropics? Impact of a latitudinal seawater δ 18 O gradient on Middle Jurassic temperature reconstructions at low latitudes
Silica diagenesis promotes early primary hydrocarbon migration
Negevite, the pyrite-type NiP 2 , a new terrestrial phosphide
Transjordanite, Ni 2 P, a new terrestrial and meteoritic phosphide, and natural solid solutions barringerite-transjordanite (hexagonal Fe 2 P–Ni 2 P)
Siwaqaite, Ca 6 Al 2 (CrO 4 ) 3 (OH) 12 ·26H 2 O, a new mineral of the ettringite group from the pyrometamorphic Daba-Siwaqa complex, Jordan
Genesis and role of bitumen in fracture development during early catagenesis
Qatranaite, CaZn 2 (OH) 6 ∙2H 2 O: a new mineral from altered pyrometamorphic rocks of the Hatrurim Complex, Daba-Siwaqa, Jordan
Removal Efficiency of Basic Blue 41 by Three Zeolites Prepared from Natural Jordanian Kaolin
Benthic Foraminifera and Geochemistry Across the Paleocene–eocene Thermal Maximum Interval in Jordan
Facies associations and chemostratigraphy of the Lower Cretaceous Kurnub Group and their boundaries, King Talal Dam section, northwestern Jordan
Abstract: Six specimens accessioned to the Bavarian State Collection for Palaeontology and Geology in Munich, Germany, in 1966 are identified as coming from a gigantic pterodactyloid pterosaur. The previously undescribed material was obtained in 1955 by Jean Otto Haas and compares favourably in size with the type specimen of the Late Cretaceous (Maastrichtian) azhdarchid pterosaur Arambourgiania philadelphiae ( Arambourg 1959 ) from the same locality/region. The material represents fragments of two cervical vertebrae, a neural arch, a left femur, a ?radius, and a metacarpal IV and bones of problematic identity, and does not duplicate the type material of Arambourgiania . The timing of its collection and its locality of Ruseifa, Jordan suggest it might pertain to the same individual as the holotype.