Onshore tsunami sediment transport mechanisms inferred from heavy mineral assemblages

The Holocene ◽  
2015 ◽  
Vol 25 (5) ◽  
pp. 795-809 ◽  
Author(s):  
Pedro JM Costa ◽  
Cesar Andrade ◽  
João Cascalho ◽  
Alastair G Dawson ◽  
Maria C Freitas ◽  
...  
Keyword(s):  
Sediment Transport ◽  
Heavy Mineral ◽  
Transport Mechanisms ◽  
Mineral Assemblages ◽  
Tsunami Sediment

Heavy mineral assemblages of the Storegga tsunami deposit

2016 ◽  
Vol 334 ◽  
pp. 21-33 ◽  
Author(s):  
J. Cascalho ◽  
P. Costa ◽  
S. Dawson ◽  
F. Milne ◽  
A. Rocha
Keyword(s):  
Heavy Mineral ◽  
Tsunami Deposit ◽  
Mineral Assemblages

Processes controlling the composition of heavy mineral assemblages in sandstones

1999 ◽  
Vol 124 (1-4) ◽  
pp. 3-29 ◽  
Author(s):  
Andrew C Morton ◽  
Claire R Hallsworth
Keyword(s):  
Heavy Mineral ◽  
Mineral Assemblages

scholarly journals Provenance of Palaeo-Rhine sediments from zircon thermochronology, geochemistry, U/Pb dating and heavy mineral assemblages

2015 ◽  
Vol 29 ◽  
pp. 396-417 ◽  
Author(s):  
Michael Tatzel ◽  
István Dunkl ◽  
Hilmar von Eynatten
Keyword(s):  
Heavy Mineral ◽  
Mineral Assemblages

On the provenance of flysch deposits in the External Hellenides of mainland Greece: results from heavy mineral studies

1998 ◽  
Vol 135 (3) ◽  
pp. 421-442 ◽  
Author(s):  
P. FAUPL ◽  
A. PAVLOPOULOS ◽  
G. MIGIROS
Keyword(s):  
Heavy Mineral ◽  
Frequent Occurrence ◽  
Chrome Spinel ◽  
Mineral Distribution ◽  
Mineral Assemblages ◽  
Subordinate Role ◽  
East West

The terrigenous materials of the flysch deposits of the External Hellenides of mainland Greece have been characterized by their heavy mineral assemblages, based on 194 samples. Three major source types were distinguished. (1) A metamorphic source is shown by abundant garnet accompanied by traces of staurolite and chloritoid. In the source of the Pindos and Ionian zones, blueschist complexes were incorporated within the metamorphic terrains, demonstrated by the frequent occurrence of blue amphiboles. (2) The existence of ophiolitic sources is indicated by the occurrence chrome spinel. Pyroxenes, green amphiboles and partly epidote are related to volcanic/metavolcanic complexes. High ophiolitic detritus was especially found in Mid-Cretaceous turbiditic layers supplied from internal terrains. (3) Granitoid and gneiss source terrains are indicated, predominantly represented by zircon, tourmaline and apatite. This type of source is characteristic for Mid-Cretaceous turbidites sampled in western parts of the Pindos zone. In the terminal flysch deposits, granitoid detritus played only a subordinate role. An extensive recycling of Pindos Flysch material into the younger Western Hellenic Flysch can be excluded. Stratigraphic trends in the heavy mineral distribution of the terminal Pindos Flysch give insights into the changing tectonic situation of the source terrains. A regional east–west trend with changing ophiolitic detritus, observed in the Parnassos-Ghiona Flysch, points to a complex feeder system.

Provenance of eolian sands in the Ulan Buh Desert, northwestern China, revealed by heavy mineral assemblages

CATENA ◽  
2020 ◽  
Vol 193 ◽  
pp. 104624 ◽  
Author(s):  
Cheng Zhang ◽  
Zhuolun Li ◽  
Qiujie Chen ◽  
Shipei Dong ◽  
Xinhui Yu ◽  
...  
Keyword(s):  
Heavy Mineral ◽  
Northwestern China ◽  
Mineral Assemblages ◽  
Ulan Buh Desert
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