GEOCHEMISTRY AND GEOCHRONOLOGY OF THE MESOZOIC VOLCANIC ROCKS IN THE SOUTHERN GREAT XINGGAN RANGE, NE CHINA
Mesozoic volcanic rocks are widespread throughout the Great Xing’an range, NE China. Their ages formed from about 180 Ma to 120 Ma, with a strong peak about 125 Ma, and several weak peaks at ∼116 Ma, ∼140 Ma and ∼156 Ma respectively in age histogram. These complicated age spectrum points out that th...
| Main Author: | |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Institute of the Earth's crust, Siberian Branch of RAS
2017-09-01
|
| Series: | Geodinamika i Tektonofizika |
| Online Access: | https://www.gt-crust.ru/jour/article/view/444 |
| id |
doaj-2d726cc6510c44fbb312c0bac617132c |
|---|---|
| record_format |
Article |
| spelling |
doaj-2d726cc6510c44fbb312c0bac617132c2021-07-29T08:39:51ZengInstitute of the Earth's crust, Siberian Branch of RASGeodinamika i Tektonofizika2078-502X2017-09-018360160210.5800/GT-2017-8-3-0303303GEOCHEMISTRY AND GEOCHRONOLOGY OF THE MESOZOIC VOLCANIC ROCKS IN THE SOUTHERN GREAT XINGGAN RANGE, NE CHINAHuaimin Xue0Institute of Geology, Chinese Academy of Geological SciencesMesozoic volcanic rocks are widespread throughout the Great Xing’an range, NE China. Their ages formed from about 180 Ma to 120 Ma, with a strong peak about 125 Ma, and several weak peaks at ∼116 Ma, ∼140 Ma and ∼156 Ma respectively in age histogram. These complicated age spectrum points out that the volcanism may be related not only with the subduction of the Pacific plate, but also with closure of the Okhotsk ocean.https://www.gt-crust.ru/jour/article/view/444 |
| collection |
DOAJ |
| language |
English |
| format |
Article |
| sources |
DOAJ |
| author |
Huaimin Xue |
| spellingShingle |
Huaimin Xue GEOCHEMISTRY AND GEOCHRONOLOGY OF THE MESOZOIC VOLCANIC ROCKS IN THE SOUTHERN GREAT XINGGAN RANGE, NE CHINA Geodinamika i Tektonofizika |
| author_facet |
Huaimin Xue |
| author_sort |
Huaimin Xue |
| title |
GEOCHEMISTRY AND GEOCHRONOLOGY OF THE MESOZOIC VOLCANIC ROCKS IN THE SOUTHERN GREAT XINGGAN RANGE, NE CHINA |
| title_short |
GEOCHEMISTRY AND GEOCHRONOLOGY OF THE MESOZOIC VOLCANIC ROCKS IN THE SOUTHERN GREAT XINGGAN RANGE, NE CHINA |
| title_full |
GEOCHEMISTRY AND GEOCHRONOLOGY OF THE MESOZOIC VOLCANIC ROCKS IN THE SOUTHERN GREAT XINGGAN RANGE, NE CHINA |
| title_fullStr |
GEOCHEMISTRY AND GEOCHRONOLOGY OF THE MESOZOIC VOLCANIC ROCKS IN THE SOUTHERN GREAT XINGGAN RANGE, NE CHINA |
| title_full_unstemmed |
GEOCHEMISTRY AND GEOCHRONOLOGY OF THE MESOZOIC VOLCANIC ROCKS IN THE SOUTHERN GREAT XINGGAN RANGE, NE CHINA |
| title_sort |
geochemistry and geochronology of the mesozoic volcanic rocks in the southern great xinggan range, ne china |
| publisher |
Institute of the Earth's crust, Siberian Branch of RAS |
| series |
Geodinamika i Tektonofizika |
| issn |
2078-502X |
| publishDate |
2017-09-01 |
| description |
Mesozoic volcanic rocks are widespread throughout the Great Xing’an range, NE China. Their ages formed from about 180 Ma to 120 Ma, with a strong peak about 125 Ma, and several weak peaks at ∼116 Ma, ∼140 Ma and ∼156 Ma respectively in age histogram. These complicated age spectrum points out that the volcanism may be related not only with the subduction of the Pacific plate, but also with closure of the Okhotsk ocean. |
| url |
https://www.gt-crust.ru/jour/article/view/444 |
| work_keys_str_mv |
AT huaiminxue geochemistryandgeochronologyofthemesozoicvolcanicrocksinthesoutherngreatxingganrangenechina |
| _version_ |
1721252778353885184 |