The article refers to the concept of use social media as an innovative tool for social capital buil-ding based on networking. It presents a modern approach to building social relationships with active parti-cipation in s...
The shallow marine deposits of the Late-Middle Jurassic (Callovian–Oxfordian) Jumara Formation of the Gangeshwar Dome of Mainland Kachchh, India, comprise a succession of ~247 m thick clastic sediments with few non-clast...
The purpose of this paper is to identify the role and nature of tax strategies used by small companies. Variable and often unpredictable market motivates businesses to seek newer and newer sources of savings. In small bu...
Upper Jurassic (Oxfordian, Bimmammatum Zone) micritic limestones show presence of omissionsurface of firmground character with trace fossils assemblage. Deformations of burrows are used to quantitative determination of m...
The Callovian and Oxfordian marine sediments of the Jaisalmer Basin constitute the uppermost part of the Jaisalmer Formation, which comprises the Kuldhar and Jajiya members. In the present paper the authors illustrate re...
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Ewa GŁOWNIAK (2004). Kolekcja J. Siemiradzkiego ze zbiorów Muzeum ING w Krakowie – fakty i refleksje. Volumina Jurassica, 2(1),
164-164. https://europub.co.uk./articles/-A-67849
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SOCIAL MEDIA AS AN INNOVATIVE TOOL SUPPORTING INNOVATION AND ENTREPRENEURSHIP
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Palaeoecologic significance of the Callovian-Oxfordian trace fossils of Gangeshwar Dome, Southeast of Bhuj, Mainland Kachchh, India
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Deformations of trace fossils versus compaction in micritic limestones, an example from Korzkiew, Upper Jurassic (Kraków Upland)
Upper Jurassic (Oxfordian, Bimmammatum Zone) micritic limestones show presence of omissionsurface of firmground character with trace fossils assemblage. Deformations of burrows are used to quantitative determination of m...
[b]Sedimentary cycles in the Callovian-Oxfordian of the Jaisalmer Basin, Rajasthan, western India[/b]
The Callovian and Oxfordian marine sediments of the Jaisalmer Basin constitute the uppermost part of the Jaisalmer Formation, which comprises the Kuldhar and Jajiya members. In the present paper the authors illustrate re...