9/11_Analysis Conclusions on Globe Triangle Concept
Important Tectonic Components of Turkey Geography based on Anatolian Plate
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I know big problems of various environment about summaried how a collision mechanism based on Anatolian Plate of Turkey Geography.Thus,this blog is reflection of 'longrange individual working efforts' completely for solution such a problem; IMPORTANT NOTE: You can observe via presentation all informations required.Also,we can summary maybe some shifting chapters for some tectonic zones(But,mainframe referencing Anatolian Plate is such a structure👍). Additionally,target mass of this presentation; Some Governors Geoengineers(to needs of almost all branches😐) Geographers(especially,researchers based on mount systems) Ekrem Erkuş Geophysics Engineer/TURKEY Update 8/1: We can say absolutely expressed unusual geologic frame of Turkey Geography considering Worldscale(6 tectonic plate stru&one trench belt stru!!!!This strs including terrestrial borders completely!Really rare example 😐); Update 12/27: Update 1/17: Other source supplementary my working based on Greece-Thraci
By the way,I established a condition check on some dbase publishes about Impact Craters...Class-2 "Duolun Structure" confirmed me.Technic informations about structure:
YanıtlaSilCountry: China (Asia)
Diameter: 70-190 km
Position: 42.05, 116.25
Age: 129 ± 2 Million Years
Drilled?:
Exposed?:
Description: Several abstracts describe a multiring impact structure ~200 km north of Beijing, China. These papers recognize inner structural ring 70 km in diameter marking occurrences of various breccias, middle ring 120 km in diameter and an outer ring 190 km in diameter. A range of various impact breccias and megabreccias, suevites, impact melt sheets with mineral fragments and microlites, aerodynamically shaped melt bombs with schlieren and fluidized ejecta have been reported but almost no data were presented to support these claims (Siben, 1987; Siben and Shuyuan, 1987; Wu and Zhang, 1987; Siben, 1989; Wu, 1989; Wu, 1990; Wu and Zhang, 1992). The target consists of granodiorite, shale siltstone, sandstone, limestone, and andesite; the andesites are of the Upper Jurasic age. Coal deposits found via drilling in the western peripheral trough (>600 m deep) is lower Cretaceous. K-Ar age of the interpreted impact melt is 129 ± 2 Ma (Siben, 1987). All data in the database are taken from (Siben, 1987). The significance of the K/Ar age is uncertain considering the lack of data on the structure. Also, if the melt sample is indeed from impact and contains fragments of minerals the K-Ar is almost certainly inaccurate. The uncertainty range listed in the database is therefore taken from the stratigraphic constraints (D. Rajmon). The base Upper Jurassic and top lower Cretaceous are calibrated with Gradstein et al. (2004).
Subject a M5.6 event(Fiji region) among tectonic region alerts during controls(expressed as triangle frame).
YanıtlaSilIn the other hand,I observed some events for NZ trench region between M4.0-M5.0 environment among descripted tectonic regions
YanıtlaSil