Deccan volcanic sequences （DYS） in the central Deccan volcanic province （CDYP） are designated as Sahyadri Group having -500 m thick lava pile associated with multiple sedimentary beds at different strati-graphic l...Deccan volcanic sequences （DYS） in the central Deccan volcanic province （CDYP） are designated as Sahyadri Group having -500 m thick lava pile associated with multiple sedimentary beds at different strati-graphic levels. In the eastern part of CDYP between the latitude 19°55-20°25 ′N and the longitudes 78°15-78° 30′E, palynological investigation of the intertrappean sedimentary beds at five stratigraphic levels was carried out. The study was basically aimed for tracking the floral and environmental changes across the Deccan transi-tion. The resulting finds indicate that the intertrappean sediments at the lowest stratigraphic level between the earliest lava flows are characterized by presence of marker Maastrichtian palynomorphs - Gabonisporis vigour- ouxii, Aquilapollenites bengalensis, Azolla cretacea and Farabeipollis associated with triporate and tricolpate pol-len grains, phytoliths of Oryzeae of Poaceae family and peridinoid dinoflagellate cysts. The increasing volcanism deteriorated the existing flora as evident by absence of pollen-spores and presence of only structured biodegraded organic matter, fungal spores, acritarchs and algal （Botryococcus） remains in the sediments of higher-up in the sequence. For chronostratigraphic constraints on the lava flows magnetic polarity of the flows bracketing the in-tertrappean beds was investigated. The results indicated presence of N-R-N-R magnetic polarity in the basal la-va pile that are interpreted as representing the magnetochron C30N to C28R （ Maastrichtian-Paleogene）. The floral change begins with the onset of volcanism in the chron C30N and floral deterioration is observed in C29N with increasing volcanism and it is only in the chron C28 R （ Danian） that some evidence of recovery of flora is recorded. The current study shows that in eastern part of CDYP the post Cretaceous-Paleogene boundary erup-tions represent the main phase of eruptions that triggered deterioration of the flora.展开更多
Since Late Proterozoic era, the Korean Peninsula has been evolved into a state with relatively stable regions and orogenic belts which were developed differently each other. The Late Paleozoie （Late Carboniferous-Ear...Since Late Proterozoic era, the Korean Peninsula has been evolved into a state with relatively stable regions and orogenic belts which were developed differently each other. The Late Paleozoie （Late Carboniferous-Early Triassic） sediments are well developed in the Korean Peninsula, and called the Pyongan System. The Pyongan System from Late Carboniferous to Lower Triassic is distributed in the Pyongnan and Hyesan-Riwon Basins, and Rangrim Massif, and divided into Hongjom （ C2 ）, Ripsok （ C2 ）, Sadong （ C2-P1 ）, Kobangsan and Rokam （Taezhawon） （P2-T1） sequences. The sediments of the Tumangang Orogenic Belt are called Tuman System which is composed of the Amgi Series, consisting of elastic formation with mafic effusive material, overlaid by the Kyeryongsan Series, consisting mainly of marie volcano sediments. The Songsang Series which rests on the Kyeryongsan Series mainly consists of elastic formation with minor felsic effusive material. In the Tumangang Orogenic Belt the tectonic movement, called Tumangang Tectonic Movement, occurred in the Lower Permian-Lower Triassic.展开更多
基金SERB-DST ( no. SR / S4 / ES619 /2012 ) for financial assistance
文摘Deccan volcanic sequences （DYS） in the central Deccan volcanic province （CDYP） are designated as Sahyadri Group having -500 m thick lava pile associated with multiple sedimentary beds at different strati-graphic levels. In the eastern part of CDYP between the latitude 19°55-20°25 ′N and the longitudes 78°15-78° 30′E, palynological investigation of the intertrappean sedimentary beds at five stratigraphic levels was carried out. The study was basically aimed for tracking the floral and environmental changes across the Deccan transi-tion. The resulting finds indicate that the intertrappean sediments at the lowest stratigraphic level between the earliest lava flows are characterized by presence of marker Maastrichtian palynomorphs - Gabonisporis vigour- ouxii, Aquilapollenites bengalensis, Azolla cretacea and Farabeipollis associated with triporate and tricolpate pol-len grains, phytoliths of Oryzeae of Poaceae family and peridinoid dinoflagellate cysts. The increasing volcanism deteriorated the existing flora as evident by absence of pollen-spores and presence of only structured biodegraded organic matter, fungal spores, acritarchs and algal （Botryococcus） remains in the sediments of higher-up in the sequence. For chronostratigraphic constraints on the lava flows magnetic polarity of the flows bracketing the in-tertrappean beds was investigated. The results indicated presence of N-R-N-R magnetic polarity in the basal la-va pile that are interpreted as representing the magnetochron C30N to C28R （ Maastrichtian-Paleogene）. The floral change begins with the onset of volcanism in the chron C30N and floral deterioration is observed in C29N with increasing volcanism and it is only in the chron C28 R （ Danian） that some evidence of recovery of flora is recorded. The current study shows that in eastern part of CDYP the post Cretaceous-Paleogene boundary erup-tions represent the main phase of eruptions that triggered deterioration of the flora.
文摘Since Late Proterozoic era, the Korean Peninsula has been evolved into a state with relatively stable regions and orogenic belts which were developed differently each other. The Late Paleozoie （Late Carboniferous-Early Triassic） sediments are well developed in the Korean Peninsula, and called the Pyongan System. The Pyongan System from Late Carboniferous to Lower Triassic is distributed in the Pyongnan and Hyesan-Riwon Basins, and Rangrim Massif, and divided into Hongjom （ C2 ）, Ripsok （ C2 ）, Sadong （ C2-P1 ）, Kobangsan and Rokam （Taezhawon） （P2-T1） sequences. The sediments of the Tumangang Orogenic Belt are called Tuman System which is composed of the Amgi Series, consisting of elastic formation with mafic effusive material, overlaid by the Kyeryongsan Series, consisting mainly of marie volcano sediments. The Songsang Series which rests on the Kyeryongsan Series mainly consists of elastic formation with minor felsic effusive material. In the Tumangang Orogenic Belt the tectonic movement, called Tumangang Tectonic Movement, occurred in the Lower Permian-Lower Triassic.
