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The C?limani Gurghiu Harghita volcanic chain East

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Eruptive history of a low-frequency and low-output rate Pleistocene volcano, Ciomadul, South Harghita Mts., Romania | SpringerLi

Ana eruption. The whole volcanic history of Ciomadul spans over ca. 1 Myr, starting with the building up of peripheral domes and then concentrating in its central part. Ciomadul appears ...

Palaeomagnetism of the Upper Miocene- Lower Pliocene lavas from the East Carpathians: contribution to the paleosecular variation of geomagnetic .

After the main collisional events at 11 Ma 9, volcanism took place in the East Carpathians forming the Călimani – Gurghiu – Harghita (CGH) volcanic chain (). ...

Source parameters of the earthquake sequence that occurred close to the BURAR array (Romania) between 24 June and 1 July 20

tration of events is visible along the Neogene volcanic chain Călimani - Gurghiu - Harghita (but only events below Mw 4.0 magnitude), located in the inner ...

Romania's earth hazards: Romania's volcanic activi

Romania's volcanic activity First and foremost, Romania has no active volcanos on its territory. But in spite of this, ... is a volcano that came about as a result of the supposed subduction along the fore land of the Carpathian chain, of the lateral movement and a ...

Tanulmányok Erdély földtanából A Kelemen-Görgényi-Hargita neogén-kvarter vulkáni ívhez kötődő ásványelőfordulások (Keleti .

neogén-kvarter vulkáni ívhez kötődő ásványelőfordulások (Keleti-Kárpátok, Románia) Mineral occurrences from the Neogene-Quaternary volcanic chain Cálimani-Gurghiu-Harghita (Eastern Carpathians, Románia) Ocuren\e minerale din lantul vulcanic neogen 1 2 3 ...

SAMPLING AND METHODS - Geod

INTRODUCTION Gurghiu Montains represent the middle segment of the 160 km-long Calimani-Gurghiu-Harghita volcanic chain located along the inner (western) side of the East Carpathian orogenic zone (Fig. 1) The volcanic chain of the Gurghiu Mountains are ...

Palaeomagnetism of the Upper Miocene- Lower Pliocene lavas from the East Carpathians: contribution to the paleosecular variation of geomagnetic .

After the main collisional events at 11 Ma 9, volcanism took place in the East Carpathians forming the Călimani – Gurghiu – Harghita (CGH) volcanic chain (). ...

Palaeomagnetism of the South Harghita volcanic rocks of the East Carpathians: implications for tectonic rotations and palaeosecular variation in .

Summary Lavas of Pliocene-Quaternary age were sampled in the South Harghita Mountains, which form the southern end of the Calimani-Gurghiu-Harghita volcanic chain of the East Carpathians. The analyses of 68 volcanic sites in the South Harghita Mountains ...

Source parameters of the earthquake sequence that occurred close to the BURAR array (Romania) between 24 June and 1 July 20

tration of events is visible along the Neogene volcanic chain Călimani - Gurghiu - Harghita (but only events below Mw 4.0 magnitude), located in the inner ...

Short movie about the gas emissions of Ciomadul volcano - YouTu

GEOCHEMISTRY AND GAS FLUX ON THE YOUNGEST VOLCANO OF THE CARPATHIAN-PANNONIAN REGION The Ciomadul volcanic system is located ant the southern end of the Calimani-Gurghiu-Harghita volcanic chain of the Eastern Carpathians, the eastern part of the Carpathian-Pannonian Region. The last eruption of the volcano occured 32 ...

B. ACTIVITIES RELATED TO DATA SYNTESIS 2. ANALYSIS AND CRITICAL DISCUSSION OF THE CURRENT MODELS ASSOCIATED TO GEODYNAMIC EVOLUTION OF THE EAST .

calc-alkaline rocks in the East Carpathians (Călimani-Gurghiu-Harghita volcanic chain); 10: Areas with active sedimentation and negative Bouguer anomaly. The following research studies evolved following two shemes: tectonic reconstruction ...

(PDF) Palaeomagnetism of the South Harghita volcanic rocks of the East Carpathians: implications for tectonic rotations and palaeosecular .

PDF | S U M M A R Y Lavas of Pliocene–Quaternary age were sampled in the South Harghita Mountains, which form the southern end of the C˘ alimani–Gurghiu–Harghita volcanic chain of the East Carpathians. The analyses of 68 volcanic sites in the South Harghita ...

(PDF) A STATISTICAL APPROACH TO THE MINERAL WATERS OF TRANSYLVANIAN BASIN-EASTERN CARPATHIANS BOUNDA

(PDF) A STATISTICAL APPROACH TO THE MINERAL WATERS OF TRANSYLVANIAN BASIN-EASTERN CARPATHIANS BOUNDARY

Geochemistry of the skarn from Mraconia Valley, Romania. | Maria Angela Anason | Request P

Request PDF on ResearchGate | On Apr 20, 2012, Maria Angela Anason and others published Geochemistry of the skarn from Mraconia Valley, Romania. We use cookies to make interactions with our website easy and meaningful, to better understand the use ...

Volcano–basement interaction in the Eastern Carpathians: Explaining unusual tectonic features in the Eastern Transylvanian Basin, Roman

Evidence of volcano–basement interaction related to the Neogene/Quaternary Călimani-Gurghiu-Harghita volcanic chain (CGH) in the Eastern Carpathians, Romania, includes both structural and morphological features. The CGH is located roughly between the ...

Volcano basement interaction in the Eastern Carpathians: Explaining unusual tectonic features in the Eastern Transylvanian Basin, Roman

Volcano–basement interaction in the Eastern Carpathians: Explaining unusual tectonic features in the ... Evidence of volcano–basement interaction related to the Neogene/Quaternary Călimani-Gurghiu-Harghita volcanic chain (CGH) in the Eastern Carpathians ...

(PDF) THICKNESS DISTRIBUTIONS AND EVOLUTION OF GROWTH MECHANISMS OF NH 4 -ILLITE FROM THE FOSSIL HYDROTHERMAL SYSTEM OF HARGHITA BA˜I, EASTERN .

Clays and Clay Minerals, Vol. 61, No. 4, 375–391, 2013. THICKNESS DISTRIBUTIONS AND EVOLUTION OF GROWTH MECHANISMS OF ˜ I, NH4-ILLITE FROM THE FOSSIL HYDROTHERMAL SYSTEM OF HARGHITA ...

Palaeomagnetism of the Upper Miocene- Lower Pliocene lavas from the East Carpathians: contribution to the paleosecular variation of geomagnetic .

After the main collisional events at 11 Ma 9, volcanism took place in the East Carpathians forming the Călimani – Gurghiu – Harghita (CGH) volcanic chain (). ...

Post-volcanic Phenomena in the East Carpathians | SpringerLi

... A. & Seghedi, I. 1995. The Calimani-Gurghiu-Harghita volcanic chain, East Carpathians, Romania: Volcanological features. Acta Vulcanologica, 7(2), 145–153 Google Scholar ...

Palaeomagnetism of the South Harghita volcanic rocks of the East Carpathians:

Abstract Lavas of Pliocene-Quaternary age were sampled in the South Harghita Mountains, which form the southern end of the Călimani-Gurghiu-Harghita volcanic chain of the East Carpathians. The analyses of 68 volcanic sites in the South Harghita Mountains ...

C LIMANI MOUNTAIN’S MONTHLY AVERAGE RUNOFF CHARACTERISTICS AND THE PROBABILITY OF ITS OCCURREN

On the northern side of the C limani Mountains from west to east string the following rivers, Dorna with Dorniúoara, Negriúoara, Neagra ùarului with Tarni a, Retitiú and Pietricelul. The Neagra ùarului River gathers its waters from ...