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The newly re-engineered G856F provides a reliable, low cost solution for a variety of magnetic search and mapping applications. Single key stroke operation means the G856F can be operated by non-technical field personnel or used in teaching environments. The G856F uses the well-established proton precession method, allowing accurate measurements to be made with virtually no dependence upon variables such as sensor orientation, temperature, or location. The unit provides a repeatable absolute total field magnetic reading, traceable to the National Institute of Standards and Technology.


The G856F is ideal for mapping geological structures, for mineral, oil and gas exploration, or magnetic search for industrial, environmental or archaeological targets, Earthquake precursor monitoring, volcanic observation, geological survey, land and marine surveying and mapping, and Iron pipe position etc. The optional gradiometer attachment gives greater resolution and noise immunity for conducting searches in high cultural noise environments. Simple operation, large digital data storage capability, and the inclusion of MagMap2000 data transfer and editing software provides a system well suited for both teaching and survey applications.
The automated cycling option with long sensor cable and external power connection allows the G856F to be used as a base station instrument for the measurement of diurnal changes in the Earth’s magnetic field. Diurnal correction data is then downloaded using MagMap2000 and can be applied to either land or airborne magnetometer data.


The G856F, based on the popular G856F, G856A and G-856AX, provides excellent performance and is the lowest priced professional magnetometer system available. With simple operation, user friendly download software, and format read for available commercial contouring programs, the G856F represents a complete magnetic surveying package generating high quality data for budget conscious users.

G856T高精度智能质子旋进磁力仪在受到激励场的激励氢核(质子)后,质子极化,当激励场去掉后,氢核(质子)会在地磁场的作用下,产生一个以地磁场方向为轴的旋进,其旋进信号的频率与地磁场强度之间有着固定关系,从而地磁场强度的测量即转化为质子旋进信号的频率测量。


根据质子在磁场中的旋进现象,因其旋进频率与磁场强度严格成正比,通过测量频率从而实现测量出磁场强度F。仪器主要由探头和操作台(主机)组成。


1、Resolution: 0.1 nT;
2、Tuning: Auto or manual, range 20000nT — 100000nT;
3、Accuracy: Absolute 0.5 nT;
4、Gradient Tolerance: 1000 nT/Meter;
5、Physical Console:18cm X 27cm X 9cm;1.6Kg;
6、Sensor: 9cm X 13cm  1.2Kg ;

1.The instrument is easy to carry, high accuracy and good stability;
2.Operation: simple hardware operation;
3.Storage: large data storage, long time data storage;
4.Automatic: data playback and processing, time interval sampling;
5.Environment: all kinds of bad weather can work normally; 6.Power: the power can be more than five days in field work;
7.Measuring range: global measurement, low latitudes measurement;
8.Function: the function covers fully G856F, G856A and G856AX;

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Current product:The newly re-engineered G856F
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Tel:(+86)010 84871775  E-mail:XL856T@126.com Add: Room 1009 Block B Peking Times Square, 103 Huizhongli Chaoyang District, Beijing China 100101

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