connate

Connate water is trapped in rock strata at the time of formation.

The pistils are composed of two to many connate carpels.

The claws are basally connate and form a tube.

Stamens can be connate (fused or joined in the same whorl).

Sepals are typically five (3-8) and more or less connate (fused) below.

The leaves are connate by flattened petioles.

The pistil consists of two connate carpels.

Non-meteoric forms of groundwater are connate water and magmatic water, also termed juvenile water.

The flowers are small with a basally connate corolla, that are imbricate or rolled up lengthwise.

Among those most commonly encountered are palmate leaves, connate sepals, and a specific structure and chemical composition of the seeds.

In the case of SP logging, the two aqueous solutions are the well bore fluid (drilling mud) and the formation water (connate water).

An understanding of the geochemistry of connate fluids is important if the diagenesis of the rock is to be quantified.

The chemical components of the connate fluid can also yield information on the provenance of aquifers and of the thermal history of the host rock.

The flowers may have 4-5 faintly connate but imbricate sepals with an equal number of distinct, imbricate petals.

There are six stamens with laterally connate filaments and oblong to ovate anthers, dorsifixed towards the base.

Whether the mud contains more or less salt than the connate water will determine the which way the SP curve will deflect opposite a permeable formation.

The pistil is made of two connate carpels, the usually superior ovary is unilocular; there is no fixed number of stamens.

Connate petals may have distinctive regions: the cylindrical base is the tube, the expanding region is the throat and the flaring outer region is the limb.

Because rock containing connate water is typically formed from ocean sediments, connate water is normally saline.

In addition to rock samples, drilling technology allows humans to obtain samples of connate fluids and of the subsurface biosphere, mostly microbial life, preserved in drilled samples.

The genus is closely related to Campanula, but has connate anthers (fused or joined in the same whorl), while Campanula species have separated anthers.

Although there are other sources of groundwater, such as connate water and magmatic water, precipitation is the major one and groundwater originated in this way is called meteoric water.

His ideas on heredity were many years ahead of their time, as this extract shows: "The offspring inherit only [their parents'] connate peculiarities and not any of the acquired qualities".

Although members of Hibiscus - an example of one of these other genera - may bear flowers with proximally connate petals, such connation occurs only at the very base of the petals.