C. Thanassoulas

发表

"Strange attractor like" electric seismic precursor observed prior to the Nafpactos, Greece, EQs of 18th / 22nd January, 2010 (Ms = 5.7R / 5.6R)

C. Thanassoulas, V. Klentos, G. Verveniotis, 2010, 1003.2772.

Geological and geophysical study of the island of Kimolos (Greece) and geothermal implications

R. O. Hansen, G. Tsokas, C. Thanassoulas, 1995 .

The nestos delta geothermal field and its relation to the associated self potential (sp) field

C. Thanassoulas, A. Lazou, 1993 .

Geothermal exploration using electrical methods

C. Thanassoulas, 1991 .

Application of the SP technique over Lagadas low enthalpy geothermal field, Greece

C. Thanassoulas, A. Lazou, 1990 .

The precursory electric signals, observed before the Izmit Turkey EQ (Mw = 7.6, August 17th, 1999), analyzed in terms of a hypothetically pre-activated, in the focal area, large scale piezoelectric mechanism

C. Thanassoulas, V. Klentos, 2011, 1111.4924.

The seismogenic area in the lithosphere considered as an "Open Physical System". Its implications on some seismological aspects. Part - I. Accelerated deformation

C. Thanassoulas, 2008, 0806.4772.

Preseismic electric signals generated by critical stress loading of the lithosphere. A review of the type of signals obtained from a long lasted (1999 to 2012) experiment conducted in Greece

C. Thanassoulas, V. Klentos, G. Verveniotis, 2012, 1209.0554.

Are charities efficient ‘firms’? A preliminary test of the UK charitable sector

J. Cullis, C. Thanassoulas, Philip Jones, 1984 .

On the recent large EQ of Karpathos, Greece (April 1st, 2011, Ms = 6.7R) and its similarities to the large EQ of the January 1st, 2006 (Ms = 6.9R) at East of Kythira, Greece

C. Thanassoulas, V. Klentos, G. Verveniotis, 2011, 1104.1368.

Geophysical investigations in the geothermal field in the delta of the Nestos river (northern Greece)

G. Tsokas, N. Kolios, C. Thanassoulas, 1987 .

Predicting West German–Comecon imports: a comparative assessment of ordinary least squares, autoregressive moving average and ridge regression procedures

C. Lawson, C. Thanassoulas, 1982 .

Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece

C. Thanassoulas, N. Xanthopoulos, 1991 .

Can large (M >= 8) EQs be triggered by tidal (M1) waves? An analysis of the global seismicity that occurred during 1901 - 2011

C. Thanassoulas, V. Klentos, G. Verveniotis, 2011, 1106.1081.

Amplitude modulated, by M1, Earth's oscillating (T = 1 day) electric field triggered by K1 tidal waves. Its relation to the occurrence time of large EQs

C. Thanassoulas, V. Klentos, G. Verveniotis, 2010, 1006.4015.

Does Global seismic energy release increase? An analysis based on the Lithospheric Seismic Energy Flow Model (LSEFM). The case of mega - earthquakes (M > 9)

C. Thanassoulas, V. Klentos, G. Verveniotis, 2012, 1210.0788.

The background seismicity rate of the Greek territory, considered as a unified seismogenic area, for the period 1964 - 2010. Is Greece in course for a large seismic event?

C. Thanassoulas, V. Klentos, G. Verveniotis, 2010, 1012.5635.

The seismogenic area in the lithosphere considered as an "Open Physical System". Its implications on some seismological aspects. Part - II. Maximum expected magnitude determination

C. Thanassoulas, 2008, 0807.0897.

Was the magnitude (M = 9.0R) of the mega-earthquake of Japan (11th of March, 2011) predictable? An analysis based on the Lithospheric Seismic Energy Flow Model (LSEFM)

C. Thanassoulas, V. Klentos, G. Verveniotis, 2012, 1204.1662.

How "Short" a "Short-term earthquake prediction" can be? A review of the case of Skyros Island,Greece, EQ (26/7/2001, Ms = 6.1 R)

C. Thanassoulas, V. Klentos, 2010, 1002.2162.

Seismic potential map of Greece calculated for the years 2005 and 2010. Its correlation to the large (Ms>=6.0R) seismic events of the 2000 - 2009 period

C. Thanassoulas, V. Klentos, 2010, 1001.1491.

The seismogenic area in the lithosphere considered as an "Open Physical System". Its implications on some seismological aspects. Part - III. Seismic Potential

C. Thanassoulas, V. Klentos, 2008, 0807.1428.

Medium - long term earthquake prediction by the use of the oscillating electric field (T = 365 days) generated due to Earth's orbit around the Sun and due to its consequent oscillating lithospheric deformation

C. Thanassoulas, V. Klentos, G. Verveniotis, 2009, 0912.0818.

Seismic electric precursors observed prior to the 6.3R EQ of July 1st 2009, Greece and their use in short-term earthquake prediction

C. Thanassoulas, V. Klentos, G. Verveniotis, 2009, 0908.4186.

On a preseismic electric field "strange attractor" like precursor observed short before large earthquakes

C. Thanassoulas, V. Klentos, G. Verveniotis, 2008, 0810.0242.

Extracting preseismic electric signals from noisy Earth's electric field data recordings. The "noise injection" method

C. Thanassoulas, V. Klentos, G. Verveniotis, 2008, 0807.4298.

Do large EQs occur randomly in time? The Mexico EQ (20th of March, 2012, Mw = 7.4) as viewed in terms of local lithospheric oscillation due to M1 and K1 tidal components. A brief presentation

C. Thanassoulas, G. Verveniotis, N. Zymaris, 2012, 1203.5286.

The Japan earthquake of March 11th, 2011 (Mw = 8.9R) as viewed in terms of local lithospheric oscillation due to M1 and K1 tidal components. A brief presentation

C. Thanassoulas, V. Klentos, G. Verveniotis, 2011, 1103.2385.

EQs ( Ms ≥ 5 . 0 R ) . A postulated theoretical physical working model and its statistical validation

C. Thanassoulas, V. Klentos, G. Verveniotis, 2011 .

Multidirectional analysis of the oscillating (T = 24 hours) Earth's electric field recorded on ground surface

C. Thanassoulas, V. Klentos, G. Verveniotis, 2008, 0808.1801.

"Short-term time prediction" of large EQs by the use of "Large Scale Piezoelectricity" generated by the focal areas loaded with excess stress load

C. Thanassoulas, 2008, 0806.0360.

Periodic variations in the Earth's electric field as earthquake precursors: Results from recent experiments in Greece

G. Tselentis, C. Thanassoulas, 1993 .

Geothermal exploration using electrical methods : Geoexploration V27, N3/4, March 1991, P321–350

C. Thanassoulas, C. Thanassoulas, 1991 .

Preseismic oscillating electric field "strange attractor" like precursor, of T=14 days, triggered by M1 tidal wave. Application on large (Ms > 6.0R) EQs in Greece (March 18th, 2006 - November 17th, 2008)

C. Thanassoulas, V. Klentos, G. Verveniotis, 2009, 0901.0467.

A PRELIMINARY RESISTIVITY INVESTIGATION (VES) OF THE LANGADA HOT SPRINGS AREA IN NORTHERN GREECE

G. Tselentis, C. Thanassoulas, G. Traganos, 1987 .

Geothermal prospecting by geoelectric soundings in NE Greece

G. Tselentis, N. Kolios, C. Thanassoulas, 1987 .

A simple BASIC program for computing terrain corrections on a microcomputer

C. Thanassoulas, Gregory N. Tsokas, G. Tsokas, 1984 .

A geothermal field model based on geophysical and thermal prospectings in Nea Kessani (NE Greece)

G. Tsokas, C. Thanassoulas, 1990 .

A deep resistivity sounding at Rookhope, Northern England

G. M. Habberjam, C. Thanassoulas, 1979, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.