Another Analysis Conclusion by Seismic Shock Thesis
Summarying perfect correlation referencing seismic shock thesis M4.4 event(W Rotorua) of Jun12 and M5.0 event(Southern Mid-Atlantic Ridge) of Jun14 with M5.3 event(N of Franz Josef Land) of Jun8 Ekrem ERKUŞ Geophysics Eng/TURKEY Update 6/23: Sensing as selective by seismic shock thesis M4.1_E Quillagua of Jun11 and M4.9_E of Severnaya Zemlya of Jun15 referencing M6.2_Western Indian-Antarctic Ridge event of Jun8 I sign to M6.2_Western Indian-Antartic Ridge event again.Expressing good correlation condition W Takotna developments of Jun13&Jun14 with M4.7_Central Mid-Atlantic Ridge of Jun7 based on event region I evaluate as a whole M4.2_SE Los Andes event of Jun3 with M4.6_S Tari event of Jun29 again referencing M4.0_SE Mostar event of June1 I observe a correlation based on M4.8_W Chonchi of Jun7 with M4.6_FarSE Kirakira of May30 referencing M4.0_SE Mostar again I referenced M4.0_SE Mostar again.Expressing perfect correlation M4.6_LosPalos Trench of May30 with M4.5_Fa...
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