Shallow lacustrine delta front （SLDF） comprises mainly sheetlike subaqueous distributary channels （SDC） formed in shallow, gentle, and tectonically steady slope （Cai and Zhu, 2011）. SDC proves an important hydro...Shallow lacustrine delta front （SLDF） comprises mainly sheetlike subaqueous distributary channels （SDC） formed in shallow, gentle, and tectonically steady slope （Cai and Zhu, 2011）. SDC proves an important hydrocarbon reservoir type in the Daqing oilfield, Changqing oilfield, and the newly discovered Moxizhuang oilfield in Central Junggar Basin. However, SDC tends to prograde quickly and move laterally frequently,展开更多
Objective The northern margin of the North China Craton (NCC),as an adjacent part between the northern NCC and the southeastern Central Asian Orogenic Belt (CAOB), has recorded multi-stage tectonic evolution information.
Objective The Makeng-type iron deposits are located in Late Paleozoic depression of southwest Fujian Province in the southeast edge of Cathaysia, which are famous for their huge scale and specific ore genesis. Previo...Objective The Makeng-type iron deposits are located in Late Paleozoic depression of southwest Fujian Province in the southeast edge of Cathaysia, which are famous for their huge scale and specific ore genesis. Previous studies mainly focus on the ore characteristics, metallogenic setting and the granites in the mining area, and there is still controversy on the ore genesis. Recent research has revealed that the iron ore bodies are spatially closely related to diabase rocks, especially those in the Makeng Fe deposit. Diabase dykes are widely distributed in the Makeng, Luoyang, Zhangkeng and other iron deposits,展开更多
There is a large Mesoproterozoic rift at the northern margin of North China Craton （NCC）, and one of China＇s most important metallogenic belts, the Langshan-Zhaertai Shan-Bayan Obo mesoproterozoic metallogenic belt...There is a large Mesoproterozoic rift at the northern margin of North China Craton （NCC）, and one of China＇s most important metallogenic belts, the Langshan-Zhaertai Shan-Bayan Obo mesoproterozoic metallogenic belt is just located in this rift. This metallogenic belt contains some large or ultra-large ore deposits, such as the Bayan Obo iron deposits and ultra-large rare earth deposits, and the large Dongshengmiao Cu-Pb-Zn sulphide deposits.展开更多
Objective Many previous researches have documented the tectonic evolution of the northern margin of North China Craton. However, whether the age of original Silurian Badangshan Formation in the study area belongs to ...Objective Many previous researches have documented the tectonic evolution of the northern margin of North China Craton. However, whether the age of original Silurian Badangshan Formation in the study area belongs to the Archean, Silurian or Devonian remains controversial, and the ductile deformation time of this formation also lack of chronological study. This work focused on the composition of the rocks in the original Silurian Badangshan Formation of the Jiefangyingzi and Dachaoyanggou area of Chifeng, and the U-Pb dating of rhyolite and late intrusive rocks, and then discussed the age of ductile deformation in order to provide new basic information for the structural evolution of this area.展开更多
基金financially supported by National Natural Science Foundation of China(Grant No.41272159 and 41372123)
文摘Shallow lacustrine delta front （SLDF） comprises mainly sheetlike subaqueous distributary channels （SDC） formed in shallow, gentle, and tectonically steady slope （Cai and Zhu, 2011）. SDC proves an important hydrocarbon reservoir type in the Daqing oilfield, Changqing oilfield, and the newly discovered Moxizhuang oilfield in Central Junggar Basin. However, SDC tends to prograde quickly and move laterally frequently,
基金the geological survey project of China Geological Survey (grant No. DD20160155 and DD20190021)
文摘Objective The northern margin of the North China Craton (NCC),as an adjacent part between the northern NCC and the southeastern Central Asian Orogenic Belt (CAOB), has recorded multi-stage tectonic evolution information.
基金financially supported by the China Geological Survey project (grants No.12120113089600, 12120114028701 and 1212011085472)
文摘Objective The Makeng-type iron deposits are located in Late Paleozoic depression of southwest Fujian Province in the southeast edge of Cathaysia, which are famous for their huge scale and specific ore genesis. Previous studies mainly focus on the ore characteristics, metallogenic setting and the granites in the mining area, and there is still controversy on the ore genesis. Recent research has revealed that the iron ore bodies are spatially closely related to diabase rocks, especially those in the Makeng Fe deposit. Diabase dykes are widely distributed in the Makeng, Luoyang, Zhangkeng and other iron deposits,
基金the project of "Properties and Metallogenic Specialization of Meso-Neopreterozoic Multiphases Rift in NCC",funded by the National Basic Research Program of China(grant No.2012CB416604)
文摘There is a large Mesoproterozoic rift at the northern margin of North China Craton （NCC）, and one of China＇s most important metallogenic belts, the Langshan-Zhaertai Shan-Bayan Obo mesoproterozoic metallogenic belt is just located in this rift. This metallogenic belt contains some large or ultra-large ore deposits, such as the Bayan Obo iron deposits and ultra-large rare earth deposits, and the large Dongshengmiao Cu-Pb-Zn sulphide deposits.
基金granted by the geological survey project of China Geological Survey (grant No.DD20160155)
文摘Objective Many previous researches have documented the tectonic evolution of the northern margin of North China Craton. However, whether the age of original Silurian Badangshan Formation in the study area belongs to the Archean, Silurian or Devonian remains controversial, and the ductile deformation time of this formation also lack of chronological study. This work focused on the composition of the rocks in the original Silurian Badangshan Formation of the Jiefangyingzi and Dachaoyanggou area of Chifeng, and the U-Pb dating of rhyolite and late intrusive rocks, and then discussed the age of ductile deformation in order to provide new basic information for the structural evolution of this area.
