Monoclinic pyrrhotite (Fe7S8) is widely claimed to carry magnetizations acquired during early diagenesis in anoxic sedimentary environments. In contrast, geochemical literature indicates that pyrrhotite formation is extremely slow below 180 °C, which ma
The low‐temperature magnetic properties of the many pyrrhotite varieties have not been studied exten...
Iron is the fourth most common element on Earth and gives rise to the magnetic properties of rock-fo...
The monosulfides of the pyrrhotite omission series (Fe$_{1−}$S, 0<≤0.125) are important remanence ca...
Monoclinic pyrrhotite (Fe7S8) is widely claimed to carry magnetizations acquired during early diagen...
[[sponsorship]]地球科學研究所[[note]]已出版;[SCI];有審查制度;具代表性[[note]]http://gateway.isiknowledge.com/gateway/Ga...
Paleomagnetic, rock magnetic, and sedimentary micro-textural data from an early Miocene mudstone seq...
Rocks associated with an orogenic gold system in the Paleoproterozoic Granites/Tanami Inlier of nort...
The monosulfides of the pyrrhotite omission series (Fe1xS; 0 < x 0:125) are important remanence carr...
Rocks associated with an orogenic gold system in the Paleoproterozoic Granites/Tanami Inlier of nort...
It is confirmed by new magnetization measurements that a magnetic transition occurs sharply at 30 K ...
International audienceDuring burial of clay-rich sediments, magnetic minerals, just as other mineral...
The sulfur-rich limit of hexagonal pyrrhotite below 290 ø C is 47.45 atomic percent iron and is inde...
Use of low temperature (LT) magnetic transitions to identify magnetic minerals that carry a remanen...
The diagenetic evolution of the magnetic minerals during burial in sedimentary basins has been recen...
Detailed rock magnetic and electron microscope analyses indicate that the magnetic signature of Neog...
The low‐temperature magnetic properties of the many pyrrhotite varieties have not been studied exten...
Iron is the fourth most common element on Earth and gives rise to the magnetic properties of rock-fo...
The monosulfides of the pyrrhotite omission series (Fe$_{1−}$S, 0<≤0.125) are important remanence ca...
Monoclinic pyrrhotite (Fe7S8) is widely claimed to carry magnetizations acquired during early diagen...
[[sponsorship]]地球科學研究所[[note]]已出版;[SCI];有審查制度;具代表性[[note]]http://gateway.isiknowledge.com/gateway/Ga...
Paleomagnetic, rock magnetic, and sedimentary micro-textural data from an early Miocene mudstone seq...
Rocks associated with an orogenic gold system in the Paleoproterozoic Granites/Tanami Inlier of nort...
The monosulfides of the pyrrhotite omission series (Fe1xS; 0 < x 0:125) are important remanence carr...
Rocks associated with an orogenic gold system in the Paleoproterozoic Granites/Tanami Inlier of nort...
It is confirmed by new magnetization measurements that a magnetic transition occurs sharply at 30 K ...
International audienceDuring burial of clay-rich sediments, magnetic minerals, just as other mineral...
The sulfur-rich limit of hexagonal pyrrhotite below 290 ø C is 47.45 atomic percent iron and is inde...
Use of low temperature (LT) magnetic transitions to identify magnetic minerals that carry a remanen...
The diagenetic evolution of the magnetic minerals during burial in sedimentary basins has been recen...
Detailed rock magnetic and electron microscope analyses indicate that the magnetic signature of Neog...
The low‐temperature magnetic properties of the many pyrrhotite varieties have not been studied exten...
Iron is the fourth most common element on Earth and gives rise to the magnetic properties of rock-fo...
The monosulfides of the pyrrhotite omission series (Fe$_{1−}$S, 0<≤0.125) are important remanence ca...