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Cretaceous Corals
The chapter gives an overview over the morphology, study methods, evolution, classification, taxonomy, and paleoecology of the post-paleozoic corals...
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Hills, Gravelly Floodplains and Peat Bogs of the Podhale—A Unique Landscape Mosaic Between the Tatra, the Beskidy and the Pieniny Mountains
The Podhale region is located between the Tatra Mountains, the Pieniny and the Beskidy Mountains in southern Poland. Its northern part—the...
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Geology of Montenegro
The territory of Montenegro belongs to the Dinarides, a tectonically active area of complex tectonic structure and lithological composition, where...
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The Rockfall Induced by Earthquake Mw 5.7 on April 22. 2022. Near Stolac City (BIH)
On the April 22, 2022. at 21:07:49 UTC, the strong earthquake with Mw 5.7 magnitude occurred on the south of Bosnia and Herzegovina. The epicenter is...
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The intracontinental High Atlas belt: geological overview and pending questions
The High Atlas intracontinental belt is an inverted rift formed along the Northwest African Craton, between the Central Atlantic Ocean and the...
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Monitoring of Groundwater Quality in Poland
Monitoring of the groundwater quality in Poland is conducted by the representatives of the Polish Geological Institute—National Research Institute...
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Intriguing Occupations at Gran Dolina (Atapuerca, Spain): the Acheulean Subunits TD10.3 and TD10.4
This paper presents the zooarchaeological, technological, use-wear, and spatial analyses of the earliest sedimentary subunits of TD10 (TD10.3 and...
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Comparative mitogenomics and phylogenetics of the family Carangidae with special emphasis on the mitogenome of the Indian Scad Decapterus russelli
Carangids are abundant and commercially important marine fish that contribute to a significant portion of the fisheries in many parts of the world....
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The South-Eastern Nida Basin (Ponidzie)—Karst in Gypsum Rocks
The south-eastern part of the Nida Basin region is the only area in Poland of gypsumGypsum karst development. Karstification, developed in several...
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Putative Triassic stem mammal Tikitherium copei is a Neogene shrew
The putative stem mammal taxon Tikitherium copei was erected based on a single tooth, identified as an upper molar, from the Upper Triassic Tiki...
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Hongshan Strike-Slip Inversion Structures and Petroleum Exploration of Qaidam Basin
Hongshan belt located in central part of Northern Qaidam basin, approximately western segment of Zongwulong mountain of Southern Qilian is composed...
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Cretaceous deposits of the northern part of the southern offshore Tanzania: depositional system, seismic manifestation, well data expressions and their implications on petroleum system elements
The northern part of the southern offshore Tanzania basin contains an operational gas field. This field is produced from the lower Cretaceous...
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The Unique Geoheritage of the Kachchh (Kutch) Basin, Western India, and its Conservation
The Kachchh Basin is a peri-cratonic rift basin in the Gujarat state of Western India which exposes a vast range of geological features which are of...
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Sequence Stratigraphy, Depositional System, and Hydrocarbon Prospectivity of the Third Rifting-Sagging Cycle in Muglad Basin
The Muglad basin, regarded as a typical passive rift, had undergone three-phase rifting-sagging cycles during Early Cretaceous, Later Cretaceous, and...
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Geomorphological Diversity of Poland—Major Controls and Main Geomorphological Regions
The chapter provides an overview of morphological diversity of Poland. Although predominantly a lowland country, Poland is remarkably diverse in...
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Frequency-Decomposed Multi-seismic-Attributes RGB Fusion Technology Applied for the Paleogene Sokor Formation Reservoir Prediction in K Area, Termit Basin, Niger
The study area K is located in the center of the Fana Low Uplift in the Termit Basin, Niger, which is known as one of hydrocarbon-prone zones in this...
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Late Cenozoic uplift of the Liupan Mountains: Evidence from the Neogene loess deposits
The Liupan Mountains, one of the important mountain ranges in western China, are located on the boundary between the northeastern Tibetan Plateau and...
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Regional Geological Characteristics of the Central African Rift System
The African Plate comprises several ancient cratonic (stable continental) nuclei. These Archean cratonic nuclei were formed 3.8–2.5 billion Ma ago....
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Oligocene Revolution
The Eocene Pelliciera mangroves were replaced by different mangrove communities dominated by Rhizophora, the precursors of modern mangroves, during...
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A comprehensive model of seismic velocities for the Bay of Mecklenburg (Baltic Sea) at the North German Basin margin: implications for basin development
The geometry of sedimentary basins is normally described by the interpretation of seismic reflectors. In addition to that, rock properties of the...
