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geophysis (seismic waves. etc) geochemistry, and some ground survying maybe?

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Geochemistry, geophysics, structural and seismology

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geophysic, geochemist, and  geology drilling are the same important techniques to study magma body

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As other classmates have previously stated, a combination of geophysics, geochemistry, structural geology, seismic interpretations, and outcrop observations are most useful when studying magma bodies. It is also important to consider geologic history and understand how magmatic bodies are impacted both by other magmatic processes or other processes such as tectonics.

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Geophysics i.e.gravity surveys and magnetotelluric surveys. Geochemistry of magmatic fluids would also help.

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Geophysics, geochemistry, and I was wondering if it would be possible to detect magma structures with seismic so that the well bores wouldn't reach magma without knowing it?

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Geophysics, geochemistry, and I was wondering if it would be possible to detect magma structures with seismic so that the well bores wouldn't reach magma without knowing it?

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Geophysics, geochemistry, structural geology, and other seismology techniques are most useful in studying and understanding magma bodies

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geochemistry, geology structures, tectonic movement and the impact of the local, geophysics, event history, analysis of the erupted rocks and modeling the chamber location.

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Geophysics (imaging of the magma), geochemistry, structural geology. Strikes and dips of contact

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A combination of geophysics, geochemistry, seismic data, isotopic dating and structural geology would be most useful.

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Forming idealised cross sections of the subsurface. If you know the rock structure beneath the surface, you could infer about magma bodies. For example, baked rock units may indicate proximity to magma, permeability/faulting is where magma may try to escape.

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Using our knowledge of geochemistry as well as field geology

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The use of drones is  another important method which allows you to look at the overall big picture. Borehole data is important also.

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geochemical analysis of rock expected to have come from the magma body under consideration, field observations paired with structural and geophysical analyses, drilling
-JB

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Field geology , geochemistry and geophysics, other techniques such as bore hole data and comparisons to other older magma bodies

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There are several techniques which others have already mentioned within their answers. These include Geochemistry, Geophysics, structural Geology, borehole data etc

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The use of geochemistry, geophysics, structural geology as mentioned by others tied in with borehole data and previous studies into magma bodies

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As said already, using geochemistry, geophysics and structural geology that has been seen in the field are the most helpful ways to look at magma bodies. This is going to give the most accurate results in terms of chemical and outcrop analysis of a particular area. If there are older magma deposits above surface, STC would be appropriate to analyse this

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I agree with my other classmates as well. Geochemical analyse at nearby springs and geospatial techniques can help with logging temperature and magnetic anomalies within the selected area. - KP

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A combination of geochemistry, geophysics and structural geology as seen in the field. The usage of drones can give a helpful 3D understanding of the geomorphology as seen in the field. Borehole data can be useful as well.

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As others have said, observation in the field and geochemical analysis of old magma bodies are useful. In addition, seismic waves sent down into the ground can help detect the location of/density of the magma in plutons; which can then be correlated to what is seen at the surface.

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As others have already said, observations in the field and use of geochemical analysis would be among the most useful techniques. Whether you are sample lava flows, or even outcrops of unerupted material (i.e. igneous suites), STCs are always a good thing to do, and testing hand samples can provide a lot of info (you could perform pXRF, etc to determine the chemistry of the rock)

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Geophysical surveys such as gravity surveys would likely play a key part in the exploration of magma bodies. Geochemistry would also be helpful through analysing the mineralogy of extruded or country rocks to determine the presence of thermal alteration, fluid inclusions or high temperature minerals.

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The combined use of geochemistry, geophysics and field observation.

Geophysics is good for determining areas of low reflectivity of a lithology composition change, and geochemistry is good for the analysis of major RRE that are present allowing an indication into the composition and magma evolution. Field observations are always good for determining a rough size and orientation of the mama bodies and also helps you understand the composition, structures and textures of the magma body.

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Geochemistry and geophysical analysis can be utilised to gain an insight to the nature of magma bodies and their movement. Field studies are also required to interpret the origin and formation of these bodies.

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Geochemistry and geophysics, using these we can find out critical info about the magma body and determine how it developed over time, such as compositions and tempuratures and pressures. 

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Geochemistry and geophysics, using these we can find out critical info about the magma body and determine how it developed over time, such as compositions and tempuratures and pressures. 

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The use of geochemistry and geophysics along with the appropriate field techniques. This will combine knowledge of old magma chambers as well as seismic activity and compositions of the exposed geothermal features.

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Surface analysis would be critical first. This would involve field observations and STCs of past flows. Also geochemistry and geophysics techniques would be necessary

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I would use field observations of old mama bodies, such as STCs, and combine that with geochemistry to try and piece together how the magma evolved. In addition, the use of geophysics to look at seismic data to try and figure how current magma bodies are behaving.

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Studying the STCs of the magma intrusions help interpret the magma bodies. Water /CO2 content and trace elements help identify the tectonic environments and crystal sizes/shapes and abundance help with analyzing the cooling environments of the magma body.

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Geochemistry and geophysics. Using these techniques we can track the magma body back to where it started to evolve and also understand the initial composition.
Gravity and seismidata may also be useful in understanding the complexity of the chamber beneath the surface

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the combination of field techniques, geochemistry and geophysics.

For example, field observations of magma chambers which have been exposed, due to erosion or found along cliffs
and then measure the length/ width of that chamber

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Geophysical studies including seismic studies - which would record movement of shallow magma bodies and gravity/density modelling

Geochemical studies- measuring chemical compositions of steam, neutral chloride waters