scholarly journals Overlapping ore mineralization of volcanic rocks from the Sea of Japan: new data

2019 ◽  
Vol 487 (1) ◽  
pp. 73-77
Author(s):  
O. N. Kolesnik ◽  
V. T. S’edin ◽  
A. N. Kolesnik ◽  
E. I. Yaroshchuk ◽  
A. A. Karabtsov
Keyword(s):  
Sea Of Japan ◽  
Volcanic Rocks ◽  
The Sea Of Japan ◽  
Rare Metals ◽  
Fluid Saturation ◽  
Mineral Phases ◽  
Ore Mineralization ◽  
First Time

An overlapping (postvolcanic) ore mineralization of volcanic rocks building up submarine edifices in the Sea of Japan has been semi-quantitatively and qualitatively evaluated for the first time. The study considers the main types of volcanic rocks (marginal continental, post-rift, and alkali ones) and focuses primarily on mineral phases formed in them by nonferrous, noble, and rare metals. The most enriched are post-rift rocks. That is due to the initial magma’s fluid saturation, as well as long-lived volcanic and postvolcanic processes.

Ore mineralization in volcanic rocks from the submarine rises of the Sea of Japan

2014 ◽  
Vol 52 (2) ◽  
pp. 144-161 ◽  
Author(s):  
N. V. Astakhova ◽  
O. N. Kolesnik ◽  
V. T. S”edin
Keyword(s):  
Sea Of Japan ◽  
Volcanic Rocks ◽  
The Sea Of Japan ◽  
Ore Mineralization

Overlapping Ore Mineralization of Volcanic Rocks from the Sea of Japan: New Data

2019 ◽  
Vol 487 (1) ◽  
pp. 786-790 ◽  
Author(s):  
O. N. Kolesnik ◽  
V. T. S’’edin ◽  
A. N. Kolesnik ◽  
E. I. Yaroshchuk ◽  
A. A. Karabtsov
Keyword(s):  
Sea Of Japan ◽  
Volcanic Rocks ◽  
The Sea Of Japan ◽  
Ore Mineralization

Deep-water Ascidiacea from the Sea of Japan

Zootaxa ◽  
2012 ◽  
Vol 3245 (1) ◽  
pp. 63 ◽  
Author(s):  
KAREN SANAMYAN ◽  
NADYA SANAMYAN
Keyword(s):  
Sea Of Japan ◽  
Deep Water ◽  
The Sea Of Japan ◽  
Genus Level ◽  
Deep Water Species ◽  
Fourth Species ◽  
First Time ◽  
Water Species

Four solitary ascidians are recorded in the deep-water material from the Sea of Japan. Two species, Agnezia orthenteronand Pelonaia bursaria are recorded for the first time since original descriptions, a third species, Styela squamosa, is awidely distributed deep-water species not known previously from the Sea of Japan. A fourth species was identified only to a genus level.

scholarly journals Early – Middle Paleozoic geology of the Sea of Japan Continent – Ocean Transitional Zone (review). Pt 2.

2020 ◽  
Author(s):  
Л.А. ИЗОСОВ ◽  
Н.П. КУЛЬКОВ
Keyword(s):  
Sea Of Japan ◽  
Western Siberia ◽  
Southern China ◽  
Transitional Zone ◽  
The Sea Of Japan ◽  
Central Asian ◽  
Continental Deposits ◽  
Middle Paleozoic ◽  
The Given ◽  
First Time

На основании обширного материала впервые проведена корреляция нижнесреднепалеозойских стратиграфических подразделений местного ранга различных регионов Япономорской зоны перехода континент–океан. Выделены стратифицирующиеся и нестратифицирующиеся магматические комплексы этих возрастов, представляющие собой вулканические, субвулканические, вулканоплутонические и плутонические образования. Авторами детально рассмотрены территориально разрозненные в основном палеонтологически охарактеризованные разрезы ордовика, силура и девона данного региона. В структурах, наложенных на докембрийские массивы, рассматриваемые отложения обычно хорошо прослеживаются по латерали, в то время как в полициклических подвижных поясах они залегают часто в виде олистолитов в мезозойских микститах или крупных ксенолитов в разновозрастных гранитоидах. Субмаринные ордовикские, силурийские и девонские отложения ЯЗ накапливались в сходной палеогеографической обстановке практически в одних и тех же седиментационных бассейнах, которые соединялись с центральноазиатскими, приохотскими и австралийскими морями. Континентальные осадки исследованной территории представлены девонскими толщами, включающими многочисленные растительные остатки, широко распространенными также в Центральном Казахстане, Западной Сибири, Приохотье и Южном Китае. On the basis of extensive material the correlation of Lower – Middle Paleozoic local-rank stratigraphic divisions of the Sea of Japan Continent – Ocean Transitional Zone is carried out for the first time. The stratified and non-stratified magmatic complexes of these ages, representing volcanic, subvolcanic, volcano-plutonic and plutonic generations are allocated. The authors have considered territorially separate, generally paleontologically characterized Ordovician, Silurian and Devonian sections of the given region in details. In the structures superimposed on Precambrian Massifs, considered sediments are usually well traced along the strike, while in Polycyclic Mobile Belts they lie down often in the form of olistoliths in Mesozoic mixtites or – large xenoliths in uneven-aged granitoids. Submarine Ordovician, Silurian and Devonian sediments of JZ accumulated in similar paleogeographic conditions, practically in the same sediment basins, which incorporated to the Central-Asian, Okhotsk and Australian Seas. Continental deposits of the investigated territory are presented by the Devonian strata, including the numerous vegetative remnants, widespread as well in the Central Kazakhstan, Western Siberia, Okhotsk Region and in Southern China.

Abnormal Winter Weather in Japan during 2012 Controlled by Large-Scale Atmospheric and Small-Scale Oceanic Phenomena

2015 ◽  
Vol 143 (1) ◽  
pp. 54-63 ◽  
Author(s):  
Yuta Ando ◽  
Masayo Ogi ◽  
Yoshihiro Tachibana
Keyword(s):  
Linear Regression ◽  
East Asia ◽  
Sea Of Japan ◽  
Large Scale ◽  
Arctic Oscillation ◽  
Small Scale ◽  
The Sea Of Japan ◽  
Interannual Variations ◽  
Regression Analyses ◽  
First Time

Abstract Negative Arctic Oscillation (AO) and western Pacific (WP) indices persisted from October to December 2012 in the Northern Hemisphere. For the first time, the monthly AO and WP were both negative for three consecutive months since records have been kept. Although in general negative AO and WP phases cause Siberia, East Asia, and Japan to be abnormally cold, Japan was relatively warm in October 2012 even though both the AO and WP were strongly negative. The temperature of the Sea of Japan reached a record-breaking high in October 2012, and it was found that heating by these very warm waters, despite the small size of the Sea of Japan, overwhelmed the cooling effect of the strongly negative AO and WP in October. Linear regression analyses showed that Japan tends to be warm in years when the Sea of Japan is warm. Consequently, the temperature over Japan is controlled by interannual variations of small-scale oceanic phenomena as well as by large-scale atmospheric patterns. Previous studies have ignored such small-scale oceanic influences on island temperatures.

Morphology of the complete larval development of the symbiotic crab Sestrostoma balssi (Shen, 1932) (Varunidae: Gaeticinae)

Zootaxa ◽  
2011 ◽  
Vol 2990 (1) ◽  
pp. 45 ◽  
Author(s):  
ELENA S. KORNIENKO ◽  
OLGA M. KORN
Keyword(s):  
Larval Development ◽  
Sea Of Japan ◽  
The Sea Of Japan ◽  
Antennal Flagellum ◽  
The Family ◽  
First Time ◽  
Russian Waters

Larval development of the symbiotic crab Sestrostoma balssi (Shen, 1932) (Varunidae: Gaeticinae) inhabiting Russian waters of the Sea of Japan is described and illustrated for the first time from material reared in the laboratory. The development includes five zoeal and a single megalopal stages. The first megalopa was attained at 20–22°C 35 days after hatching. The present paper is the first description of the complete larval development in the genus Sestrostoma. The larvae of S. balssi share all principal characters of the family Varunidae but are distinguished from the typical varunid larvae by the absence of a well-developed antennal exopod in the zoea and the presence of an 8-segmented antennal flagellum in the megalopa.

The larval development of the mud shrimp Upogebia issaeffi (Balss, 1913) (Decapoda: Gebiidea: Upogebiidae) reared under laboratory conditions

Zootaxa ◽  
2012 ◽  
Vol 3269 (1) ◽  
pp. 31 ◽  
Author(s):  
ELENA S. KORNIENKO ◽  
OLGA M. KORN ◽  
DARYA D. DEMCHUK
Keyword(s):  
Larval Development ◽  
Sea Of Japan ◽  
Zoeal Stage ◽  
The Sea Of Japan ◽  
Laboratory Conditions ◽  
Mud Shrimp ◽  
First Time ◽  
Russian Waters

Larval development of the mud shrimp Upogebia issaeffi (Balss, 1913) (Decapoda: Gebiidea: Upogebiidae) is describedand illustrated for the first time from material reared in the laboratory. The development includes four zoeal and a singlemegalopal stages. At 20–22°C the first megalopa was attained 12 days after hatching. U. issaeffi is distinguished from U.major, the second upogebiid species inhabiting Russian waters of the Sea of Japan, by the presence of the fourth zoeal stage and considerably more intensive larval setation.

scholarly journals Hydrothermal formations of pervenets rise (the Sea of Japan)

2019 ◽  
pp. 29-39
Author(s):  
N. V. Astakhova ◽  
E. A. Lopatnikov ◽  
A. V. Mozherovsky ◽  
E. I. Jaroshhuk
Keyword(s):  
Chemical Composition ◽  
Sea Of Japan ◽  
Volcanic Rocks ◽  
The Sea Of Japan ◽  
Hydrothermal Solutions ◽  
Local Distribution ◽  
Crust Structure

The data are given on the structure, chemical composition, and content of microelements in the ferromanganese and siliceous crusts of Pervenets Rise (the Sea of Japan). The crusts resulted from the cementation of small fragments of green clays (celadonite) with hydroxides of manganese (todorokite and birnessite) or silica. Initial was the formation of celadonite deposited during the eruption of ore-bearing hydrothermal solutions in the volcano caldera or on its slopes.The features of the crust structure show that they were originated through the diffusive infiltration of gas-hydrothermal solutions along the fractures or weakened zones in volcanic rocks and subsequent cementation of the celadonite already formed occurrences with manganese or siliceous oxides. The manganese and siliceous mineralization is separated in time and often in space and demonstrate more local distribution.

Cyclostome bryozoans from Qingdao, South Yellow Sea, China

Zootaxa ◽  
2019 ◽  
Vol 4603 (3) ◽  
pp. 473
Author(s):  
H. LIU ◽  
X. LIU ◽  
K. ZÁGORŠEK
Keyword(s):  
Sea Of Japan ◽  
Yellow Sea ◽  
Western Pacific ◽  
The Sea Of Japan ◽  
South Yellow Sea ◽  
Additional Species ◽  
First Time ◽  
The Western Pacific

Twenty-one species of cyclostome bryozoans are described from the coast of Qingdao (South Yellow Sea, China), belonging to 11 genera (Filicrisia, Crisia, Tubulipora, Exidmonea, Idmidronea, Qingdaoella n. gen., Nevianipora, Hemipustulopora, Microeciella, Patinella and Disporella). One genus (Qingdaoella n. gen.) and 10 species are new, while an additional species is reported for the first time from China. The most similar bryozoan assemblages to the Chinese cyclostomes described here are reported from the Sea of Japan and the western Pacific.

scholarly journals FORTIFICATIONS IN THE AVVAKUMOVKA RIVER BASININ EASTERN PRIMORYE

2020 ◽  
Author(s):  
О.В. Дьякова
Keyword(s):  
River Basin ◽  
Sea Of Japan ◽  
Field Research ◽  
Mountain Pass ◽  
The Sea Of Japan ◽  
Medieval Period ◽  
First Time

В статье на основе архивных источников и полевых исследований предлагается картирование и классификация девяти древних и средневековых укреплений бассейна р. Аввакумовки Восточного Приморья (Ольгинский район Приморского края). По геоморфологической характеристике укрепления относятся к мысовому, долинному и горному типам. Установлено, что фортификационные памятники создавались носителями разных культур (янковской, польцевской, мохэской, чжурчжэньской), датируемых I тыс. до н. э. – первой половиной II тыс. н. э. Впервые выявлено, что Михайловское городище относится к польцевской культуре эпохи Средневековья (VI в. н. э.). Расположение укреплений вдоль реки и ее притоков свидетельствует о функционировании здесь сухопутной и морской дорог. Сухопутная дорога спускалась с перевала к морю, морская магистраль пролегала вдоль побережья Японского моря. Based on archival sources and field research, the paper offers mapping and classification of nine ancient and medieval fortifications located in the Avvakumovka River basin in Eastern Primorye (Olga district of Primorye). Regarding their geomorphological characteristics, the fortifications are referred to promontory, valley and mountainous types. It has been discovered that the fortifications were built by people representing various cultures (the Yankovka, the Poltse, the Mohe, the Jurchen cultures) dating to I mill. BC – first half of II mill. AD. It has been established for the first time that the Mikhaylovskoye fortified settlement is attributed to the Poltse culture of the medieval period (6th century). The location of the fortifications along the river and its tributaries suggest existence of local overland and marine roads. The overland road descended from a mountain pass to the sea, whereas the marine road ran along the coastline of the sea of Japan.

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